Granite genesis: in-situ melting and crustal evolution
This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of ab...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chen, Guo-Neng [verfasserIn] |
|---|
| Format: |
E-Book |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
Dordrecht: Springer Science+Business Media B.V ; 2007 |
|---|
| Schlagwörter: |
Kontinentale Erdkruste / Granitische Schmelze / Granit / Gesteinsbildung / Gesteinskunde |
|---|---|
| Schlagwörter: |
| Anmerkung: |
Includes bibliographical references and index |
|---|---|
| Umfang: |
Online-Ressource ; v.: digital |
| Reproduktion: |
Online-Ausg. ; Springer eBook Collection. Earth and Environmental Science |
|---|
| Links: | |
|---|---|
| ISBN: |
978-1-4020-5891-2 |
| DOI / URN: |
10.1007/978-1-4020-5891-2 |
|---|
| Katalog-ID: |
55011985X |
|---|
| LEADER | 01000cam a22002652 4500 | ||
|---|---|---|---|
| 001 | 55011985X | ||
| 003 | DE-627 | ||
| 005 | 20240226132524.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 071122s2007 ne |||||o 00| ||eng c | ||
| 020 | |a 9781402058912 |9 978-1-4020-5891-2 | ||
| 024 | 7 | |a 10.1007/978-1-4020-5891-2 |2 doi | |
| 035 | |a (DE-627)55011985X | ||
| 035 | |a (DE-599)GBV55011985X | ||
| 035 | |a (OCoLC)315762962 | ||
| 035 | |a (DE-He213)978-1-4020-5891-2 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 044 | |c XA-NL | ||
| 050 | 0 | |a QE462.G7 | |
| 082 | 0 | |a 552.3 |2 22 | |
| 082 | 0 | 4 | |a 550 |
| 084 | |a 38.26 |2 bkl | ||
| 084 | |a 38.36 |2 bkl | ||
| 100 | 1 | |a Chen, Guo-Neng |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Granite genesis: in-situ melting and crustal evolution |c edited by Guo-Neng Chen, Rodney Grapes |
| 264 | 1 | |a Dordrecht |b Springer Science+Business Media B.V |c 2007 | |
| 300 | |a Online-Ressource |b v.: digital | ||
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 500 | |a Includes bibliographical references and index | ||
| 505 | 8 | 0 | |a FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf |
| 520 | |a This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. | ||
| 520 | |a Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology | ||
| 530 | |a Electronic reproduction; Available via World Wide Web | ||
| 533 | |a Online-Ausg. |f Springer eBook Collection. Earth and Environmental Science |n Electronic reproduction; Available via World Wide Web | ||
| 650 | 0 | |a Geochemistry | |
| 650 | 0 | |a Geology | |
| 650 | 0 | |a Physical geography | |
| 650 | 0 | |a Mineralogy | |
| 689 | 0 | 0 | |D s |0 (DE-588)4451364-1 |0 (DE-627)227154967 |0 (DE-576)212575198 |a Kontinentale Erdkruste |2 gnd |
| 689 | 0 | 1 | |D s |0 (DE-588)4158036-9 |0 (DE-627)105496138 |0 (DE-576)209839082 |a Granitische Schmelze |2 gnd |
| 689 | 0 | 2 | |D s |0 (DE-588)4132750-0 |0 (DE-627)105685321 |0 (DE-576)209638192 |a Granit |2 gnd |
| 689 | 0 | 3 | |D s |0 (DE-588)4157153-8 |0 (DE-627)104130911 |0 (DE-576)209832223 |a Gesteinsbildung |2 gnd |
| 689 | 0 | 4 | |D s |0 (DE-588)4020740-7 |0 (DE-627)106316915 |0 (DE-576)208934626 |a Gesteinskunde |2 gnd |
| 689 | 0 | |5 (DE-627) | |
| 700 | 1 | |a Grapes, Rodney |4 oth | |
| 776 | 1 | |z 9781402058905 | |
| 856 | 4 | 0 | |u http://dx.doi.org/10.1007/978-1-4020-5891-2 |x Resolving-System |z lizenzpflichtig |3 Volltext |
| 856 | 4 | 2 | |u http://www.gbv.de/dms/bowker/toc/9781402058905.pdf |m V:DE-601 |m X:Bowker |q pdf/application |v 2011-12-23 |x Verlag |y Inhaltsverzeichnis |3 Inhaltsverzeichnis |
| 912 | |a ZDB-2-EES |b 2007 | ||
| 912 | |a GBV_ILN_23 | ||
| 912 | |a ISIL_DE-830 | ||
| 912 | |a SYSFLAG_1 | ||
| 912 | |a GBV_KXP | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a SSG-OPC-GEO | ||
| 912 | |a GBV_ILN_60 | ||
| 912 | |a ISIL_DE-705 | ||
| 912 | |a GBV_ILN_65 | ||
| 912 | |a ISIL_DE-3 | ||
| 912 | |a GBV_ILN_120 | ||
| 912 | |a ISIL_DE-715 | ||
| 912 | |a GBV_ILN_370 | ||
| 912 | |a ISIL_DE-1373 | ||
| 936 | b | k | |a 38.26 |j Magmatische Gesteine |0 (DE-627)10640718X |
| 936 | b | k | |a 38.36 |j Tektonik |0 (DE-627)106407147 |
| 951 | |a BO | ||
| 953 | |2 045F |a 552.3 | ||
| 980 | |2 23 |1 01 |x 0830 |b 852490046 |c 00 |f --%%-- |d --%%-- |e s |j --%%-- |h olr-springer |u i |y z |z 12-12-07 | ||
| 980 | |2 60 |1 01 |x 0705 |b 4304949497 |h SpringerLink |k Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. |k Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung |y z |z 07-04-23 | ||
| 980 | |2 65 |1 01 |x 0003 |b 1655656309 |c 03 |f --%%-- |d ebook |e --%%-- |j --%%-- |h OLR-SEB-ZDB-2-EES |k Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. |y k3o |z 02-01-17 | ||
| 980 | |2 120 |1 01 |x 0715 |b 1840105739 |h OLR-ESP |k Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. |y z |z 13-01-19 | ||
| 980 | |2 120 |1 02 |x 0715 |b 357768481X |c 00 |f --%%-- |d --%%-- |e g |j --%%-- |h alma |y z |z 21-01-20 | ||
| 980 | |2 370 |1 01 |x 4370 |b 1845236394 |h olr-springer |k Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. |u i |y z |z 27-01-19 | ||
| 981 | |2 23 |1 01 |x 0830 |y Springer EBook |r http://dx.doi.org/10.1007/978-1-4020-5891-2 | ||
| 981 | |2 60 |1 01 |x 0705 |y Volltextzugang Campus |r http://dx.doi.org/10.1007/978-1-4020-5891-2 | ||
| 981 | |2 65 |1 01 |x 0003 |y Volltextzugang Campus |r http://dx.doi.org/10.1007/978-1-4020-5891-2 | ||
| 981 | |2 120 |1 01 |x 0715 |r http://dx.doi.org/10.1007/978-1-4020-5891-2 | ||
| 981 | |2 120 |1 02 |x 0715 |r http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 | ||
| 981 | |2 370 |1 01 |x 4370 |y E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich |r http://dx.doi.org/10.1007/978-1-4020-5891-2 | ||
| 983 | |2 120 |1 00 |x DE-715 |8 99 |a ww | ||
| 985 | |2 23 |1 01 |x 0830 |a 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 | ||
| 985 | |2 120 |1 01 |x 0715 |a YH 2020 | ||
| 995 | |2 23 |1 01 |x 0830 |a olr-springer | ||
| 995 | |2 60 |1 01 |x 0705 |a SpringerLink | ||
| 995 | |2 65 |1 01 |x 0003 |a OLR-SEB-ZDB-2-EES | ||
| 995 | |2 120 |1 01 |x 0715 |a OLR-ESP | ||
| 995 | |2 120 |1 02 |x 0715 |a alma | ||
| 995 | |2 370 |1 01 |x 4370 |a olr-springer | ||
| 998 | |2 23 |1 01 |x 0830 |0 2007.12.12 | ||
| matchkey_str |
book:9781402058912:2007---- |
|---|---|
| oclc_num |
315762962 |
| publishDate |
2007 |
| building |
23 60 65:3 120 370 |
| topic_facet |
Geochemistry Geology Physical geography Mineralogy Kontinentale Erdkruste Granitische Schmelze Granit Gesteinsbildung Gesteinskunde |
| isfreeaccess_bool |
false |
| publishDateDaySort_date |
2007-01-01T00:00:00Z |
| dewey-sort |
3552.3 |
| id |
55011985X |
| signature_iln |
65:ebook 0003:ebook |
| signature_iln_str_mv |
65:ebook 0003:ebook |
| signature_iln_scis_mv |
65:ebook 0003:ebook |
| language_de |
englisch |
| standort_str_mv |
--%%-- |
| callnumber-first |
Q - Science |
| dewey-ones |
552 - Petrology 550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| publishPlace |
Dordrecht |
| callnumber-label |
QE462 |
| last_changed_iln_str_mv |
23@12-12-07 60@07-04-23 65@02-01-17 120@13-01-19 120@21-01-20 370@27-01-19 |
| illustrated |
Not Illustrated |
| contents |
FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf |
| spellingShingle |
FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf Chen, Guo-Neng misc QE462.G7 ddc 552.3 ddc 550 bkl 38.26 bkl 38.36 misc Geochemistry misc Geology misc Physical geography misc Mineralogy gnd Kontinentale Erdkruste gnd Granitische Schmelze gnd Granit gnd Gesteinsbildung gnd Gesteinskunde Granite genesis: in-situ melting and crustal evolution |
| topic_title |
QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) |
| format_facet |
Elektronische Bücher Bücher Elektronische Ressource |
| standort_txtP_mv |
--%%-- |
| signature |
--%%-- ebook |
| signature_str_mv |
--%%-- ebook |
| isfreeaccess_txt |
false |
| normlinkwithrole_str_mv |
(DE-588)4451364-1@@689@@ (DE-588)4158036-9@@689@@ (DE-588)4132750-0@@689@@ (DE-588)4157153-8@@689@@ (DE-588)4020740-7@@689@@ |
| ctrlnum |
(DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 |
| title_full |
Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes |
| author_sort |
Chen, Guo-Neng |
| isOA_bool |
false |
| publishDateSort |
2007 |
| selectkey |
23:z 60:z 65:k 120:z 370:z |
| format_se |
Elektronische Bücher |
| countryofpublication_str_mv |
XA-NL |
| author-letter |
Chen, Guo-Neng |
| doi_str_mv |
10.1007/978-1-4020-5891-2 |
| dewey-full |
552.3 550 |
| title_sort |
granite genesis: in-situ melting and crustal evolution |
| title_auth |
Granite genesis: in-situ melting and crustal evolution |
| abstract |
This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Includes bibliographical references and index |
| abstractGer |
This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Includes bibliographical references and index |
| abstract_unstemmed |
This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Includes bibliographical references and index |
| url |
http://dx.doi.org/10.1007/978-1-4020-5891-2 http://www.gbv.de/dms/bowker/toc/9781402058905.pdf |
| author2 |
Grapes, Rodney |
| author2Str |
Grapes, Rodney |
| callnumber-subject |
QE - Geology |
| mediatype_str_mv |
c |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth |
| author_variant |
g n c gnc |
| hierarchy_sort_str |
2007 |
| bklnumber |
38.26 38.36 |
| callnumber-subject-code |
QE |
| allfields |
9781402058912 978-1-4020-5891-2 10.1007/978-1-4020-5891-2 doi (DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 DE-627 ger DE-627 rakwb eng XA-NL QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Chen, Guo-Neng verfasserin aut Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Dordrecht Springer Science+Business Media B.V 2007 Online-Ressource v.: digital Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Includes bibliographical references and index FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Electronic reproduction; Available via World Wide Web Online-Ausg. Springer eBook Collection. Earth and Environmental Science Electronic reproduction; Available via World Wide Web Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) Grapes, Rodney oth 9781402058905 http://dx.doi.org/10.1007/978-1-4020-5891-2 Resolving-System lizenzpflichtig Volltext http://www.gbv.de/dms/bowker/toc/9781402058905.pdf V:DE-601 X:Bowker pdf/application 2011-12-23 Verlag Inhaltsverzeichnis Inhaltsverzeichnis ZDB-2-EES 2007 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 38.26 Magmatische Gesteine (DE-627)10640718X 38.36 Tektonik (DE-627)106407147 BO 045F 552.3 23 01 0830 852490046 00 --%%-- --%%-- s --%%-- olr-springer i z 12-12-07 60 01 0705 4304949497 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655656309 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840105739 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 357768481X 00 --%%-- --%%-- g --%%-- alma z 21-01-20 370 01 4370 1845236394 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 27-01-19 23 01 0830 Springer EBook http://dx.doi.org/10.1007/978-1-4020-5891-2 60 01 0705 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 65 01 0003 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 120 01 0715 http://dx.doi.org/10.1007/978-1-4020-5891-2 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich http://dx.doi.org/10.1007/978-1-4020-5891-2 120 00 DE-715 99 ww 23 01 0830 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2007.12.12 |
| spelling |
9781402058912 978-1-4020-5891-2 10.1007/978-1-4020-5891-2 doi (DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 DE-627 ger DE-627 rakwb eng XA-NL QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Chen, Guo-Neng verfasserin aut Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Dordrecht Springer Science+Business Media B.V 2007 Online-Ressource v.: digital Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Includes bibliographical references and index FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Electronic reproduction; Available via World Wide Web Online-Ausg. Springer eBook Collection. Earth and Environmental Science Electronic reproduction; Available via World Wide Web Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) Grapes, Rodney oth 9781402058905 http://dx.doi.org/10.1007/978-1-4020-5891-2 Resolving-System lizenzpflichtig Volltext http://www.gbv.de/dms/bowker/toc/9781402058905.pdf V:DE-601 X:Bowker pdf/application 2011-12-23 Verlag Inhaltsverzeichnis Inhaltsverzeichnis ZDB-2-EES 2007 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 38.26 Magmatische Gesteine (DE-627)10640718X 38.36 Tektonik (DE-627)106407147 BO 045F 552.3 23 01 0830 852490046 00 --%%-- --%%-- s --%%-- olr-springer i z 12-12-07 60 01 0705 4304949497 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655656309 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840105739 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 357768481X 00 --%%-- --%%-- g --%%-- alma z 21-01-20 370 01 4370 1845236394 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 27-01-19 23 01 0830 Springer EBook http://dx.doi.org/10.1007/978-1-4020-5891-2 60 01 0705 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 65 01 0003 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 120 01 0715 http://dx.doi.org/10.1007/978-1-4020-5891-2 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich http://dx.doi.org/10.1007/978-1-4020-5891-2 120 00 DE-715 99 ww 23 01 0830 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2007.12.12 |
| allfields_unstemmed |
9781402058912 978-1-4020-5891-2 10.1007/978-1-4020-5891-2 doi (DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 DE-627 ger DE-627 rakwb eng XA-NL QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Chen, Guo-Neng verfasserin aut Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Dordrecht Springer Science+Business Media B.V 2007 Online-Ressource v.: digital Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Includes bibliographical references and index FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Electronic reproduction; Available via World Wide Web Online-Ausg. Springer eBook Collection. Earth and Environmental Science Electronic reproduction; Available via World Wide Web Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) Grapes, Rodney oth 9781402058905 http://dx.doi.org/10.1007/978-1-4020-5891-2 Resolving-System lizenzpflichtig Volltext http://www.gbv.de/dms/bowker/toc/9781402058905.pdf V:DE-601 X:Bowker pdf/application 2011-12-23 Verlag Inhaltsverzeichnis Inhaltsverzeichnis ZDB-2-EES 2007 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 38.26 Magmatische Gesteine (DE-627)10640718X 38.36 Tektonik (DE-627)106407147 BO 045F 552.3 23 01 0830 852490046 00 --%%-- --%%-- s --%%-- olr-springer i z 12-12-07 60 01 0705 4304949497 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655656309 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840105739 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 357768481X 00 --%%-- --%%-- g --%%-- alma z 21-01-20 370 01 4370 1845236394 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 27-01-19 23 01 0830 Springer EBook http://dx.doi.org/10.1007/978-1-4020-5891-2 60 01 0705 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 65 01 0003 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 120 01 0715 http://dx.doi.org/10.1007/978-1-4020-5891-2 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich http://dx.doi.org/10.1007/978-1-4020-5891-2 120 00 DE-715 99 ww 23 01 0830 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2007.12.12 |
| allfieldsGer |
9781402058912 978-1-4020-5891-2 10.1007/978-1-4020-5891-2 doi (DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 DE-627 ger DE-627 rakwb eng XA-NL QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Chen, Guo-Neng verfasserin aut Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Dordrecht Springer Science+Business Media B.V 2007 Online-Ressource v.: digital Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Includes bibliographical references and index FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Electronic reproduction; Available via World Wide Web Online-Ausg. Springer eBook Collection. Earth and Environmental Science Electronic reproduction; Available via World Wide Web Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) Grapes, Rodney oth 9781402058905 http://dx.doi.org/10.1007/978-1-4020-5891-2 Resolving-System lizenzpflichtig Volltext http://www.gbv.de/dms/bowker/toc/9781402058905.pdf V:DE-601 X:Bowker pdf/application 2011-12-23 Verlag Inhaltsverzeichnis Inhaltsverzeichnis ZDB-2-EES 2007 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 38.26 Magmatische Gesteine (DE-627)10640718X 38.36 Tektonik (DE-627)106407147 BO 045F 552.3 23 01 0830 852490046 00 --%%-- --%%-- s --%%-- olr-springer i z 12-12-07 60 01 0705 4304949497 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655656309 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840105739 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 357768481X 00 --%%-- --%%-- g --%%-- alma z 21-01-20 370 01 4370 1845236394 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 27-01-19 23 01 0830 Springer EBook http://dx.doi.org/10.1007/978-1-4020-5891-2 60 01 0705 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 65 01 0003 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 120 01 0715 http://dx.doi.org/10.1007/978-1-4020-5891-2 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich http://dx.doi.org/10.1007/978-1-4020-5891-2 120 00 DE-715 99 ww 23 01 0830 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2007.12.12 |
| allfieldsSound |
9781402058912 978-1-4020-5891-2 10.1007/978-1-4020-5891-2 doi (DE-627)55011985X (DE-599)GBV55011985X (OCoLC)315762962 (DE-He213)978-1-4020-5891-2 DE-627 ger DE-627 rakwb eng XA-NL QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl Chen, Guo-Neng verfasserin aut Granite genesis: in-situ melting and crustal evolution edited by Guo-Neng Chen, Rodney Grapes Dordrecht Springer Science+Business Media B.V 2007 Online-Ressource v.: digital Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Includes bibliographical references and index FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology Electronic reproduction; Available via World Wide Web Online-Ausg. Springer eBook Collection. Earth and Environmental Science Electronic reproduction; Available via World Wide Web Geochemistry Geology Physical geography Mineralogy s (DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 Kontinentale Erdkruste gnd s (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 Granitische Schmelze gnd s (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 Granit gnd s (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 Gesteinsbildung gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) Grapes, Rodney oth 9781402058905 http://dx.doi.org/10.1007/978-1-4020-5891-2 Resolving-System lizenzpflichtig Volltext http://www.gbv.de/dms/bowker/toc/9781402058905.pdf V:DE-601 X:Bowker pdf/application 2011-12-23 Verlag Inhaltsverzeichnis Inhaltsverzeichnis ZDB-2-EES 2007 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 38.26 Magmatische Gesteine (DE-627)10640718X 38.36 Tektonik (DE-627)106407147 BO 045F 552.3 23 01 0830 852490046 00 --%%-- --%%-- s --%%-- olr-springer i z 12-12-07 60 01 0705 4304949497 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655656309 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840105739 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 357768481X 00 --%%-- --%%-- g --%%-- alma z 21-01-20 370 01 4370 1845236394 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 27-01-19 23 01 0830 Springer EBook http://dx.doi.org/10.1007/978-1-4020-5891-2 60 01 0705 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 65 01 0003 Volltextzugang Campus http://dx.doi.org/10.1007/978-1-4020-5891-2 120 01 0715 http://dx.doi.org/10.1007/978-1-4020-5891-2 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich http://dx.doi.org/10.1007/978-1-4020-5891-2 120 00 DE-715 99 ww 23 01 0830 2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2007.12.12 |
| language |
English |
| format_phy_str_mv |
Book |
| bklname |
Magmatische Gesteine Tektonik |
| institution |
findex.gbv.de |
| selectbib_iln_str_mv |
23@ 60@ 65@3o 120@ 370@ |
| dewey-raw |
552.3 |
| authorswithroles_txt_mv |
Chen, Guo-Neng @@aut@@ Grapes, Rodney @@oth@@ |
| series2 |
Springer eBook Collection. Earth and Environmental Science |
| standort_iln_str_mv |
23:--%%-- 0830:--%%-- 65:--%%-- 0003:--%%-- 120:--%%-- 0715:--%%-- |
| author |
Chen, Guo-Neng |
| authorStr |
Chen, Guo-Neng |
| format |
eBook |
| typewithnormlink_str_mv |
SubjectHeadingSensoStricto@(DE-588)4451364-1 SubjectHeading@(DE-588)4451364-1 SubjectHeading@(DE-588)4158036-9 SubjectHeadingSensoStricto@(DE-588)4158036-9 SubjectHeading@(DE-588)4132750-0 SubjectHeadingSensoStricto@(DE-588)4132750-0 SubjectHeading@(DE-588)4157153-8 SubjectHeadingSensoStricto@(DE-588)4157153-8 SubjectHeadingSensoStricto@(DE-588)4020740-7 SubjectHeading@(DE-588)4020740-7 |
| collection |
KXP GVK |
| remote_str |
true |
| abrufzeichen_iln_str_mv |
23@olr-springer 60@SpringerLink 65@OLR-SEB-ZDB-2-EES 120@OLR-ESP 120@alma 370@olr-springer |
| abrufzeichen_iln_scis_mv |
23@olr-springer 60@SpringerLink 65@OLR-SEB-ZDB-2-EES 120@OLR-ESP 120@alma 370@olr-springer |
| notation_local_iln_str_mv |
120:ww DE-715:ww |
| publisher |
Springer Science+Business Media B.V |
| publisherStr |
Springer Science+Business Media B.V |
| topic |
misc QE462.G7 ddc 552.3 ddc 550 bkl 38.26 bkl 38.36 misc Geochemistry misc Geology misc Physical geography misc Mineralogy gnd Kontinentale Erdkruste gnd Granitische Schmelze gnd Granit gnd Gesteinsbildung gnd Gesteinskunde |
| topic_unstemmed |
misc QE462.G7 ddc 552.3 ddc 550 bkl 38.26 bkl 38.36 misc Geochemistry misc Geology misc Physical geography misc Mineralogy gnd Kontinentale Erdkruste gnd Granitische Schmelze gnd Granit gnd Gesteinsbildung gnd Gesteinskunde |
| topic_browse |
misc QE462.G7 ddc 552.3 ddc 550 bkl 38.26 bkl 38.36 misc Geochemistry misc Geology misc Physical geography misc Mineralogy gnd Kontinentale Erdkruste gnd Granitische Schmelze gnd Granit gnd Gesteinsbildung gnd Gesteinskunde |
| format_main_str_mv |
Text Buch |
| carriertype_str_mv |
cr |
| author2_variant |
r g rg |
| normlinkwithtype_str_mv |
(DE-588)4451364-1@SubjectHeadingSensoStricto (DE-588)4451364-1@SubjectHeading (DE-588)4158036-9@SubjectHeading (DE-588)4158036-9@SubjectHeadingSensoStricto (DE-588)4132750-0@SubjectHeading (DE-588)4132750-0@SubjectHeadingSensoStricto (DE-588)4157153-8@SubjectHeading (DE-588)4157153-8@SubjectHeadingSensoStricto (DE-588)4020740-7@SubjectHeadingSensoStricto (DE-588)4020740-7@SubjectHeading |
| dewey-tens |
550 - Earth sciences & geology |
| isbn |
9781402058912 1402058918 9781402058905 140205890X |
| title |
Granite genesis: in-situ melting and crustal evolution |
| exemplarkommentar_str_mv |
60@Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. 60@Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung 65@Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. 120@Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. 370@Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. |
| callnumber-first-code |
Q |
| lang_code |
eng |
| class_local |
120 00 DE-715 99 ww |
| selektneu_str_mv |
23@2007.12.12 |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| contenttype_str_mv |
txt |
| class_local_iln |
120:ww DE-715:ww |
| author_browse |
Chen, Guo-Neng |
| physical |
Online-Ressource v.: digital |
| class |
QE462.G7 552.3 22 550 38.26 bkl 38.36 bkl 120 00 DE-715 99 ww |
| classname_local_iln_str_mv |
120: DE-715: |
| normlink |
4451364-1 227154967 212575198 4158036-9 105496138 209839082 4132750-0 105685321 209638192 4157153-8 104130911 209832223 4020740-7 106316915 208934626 10640718X 106407147 2007.12.12 |
| normlink_prefix_str_mv |
(DE-588)4451364-1 (DE-627)227154967 (DE-576)212575198 (DE-588)4158036-9 (DE-627)105496138 (DE-576)209839082 (DE-588)4132750-0 (DE-627)105685321 (DE-576)209638192 (DE-588)4157153-8 (DE-627)104130911 (DE-576)209832223 (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 (DE-627)10640718X (DE-627)106407147 2007.12.12 |
| callnumber |
QE462.G7 |
| collection_details |
ZDB-2-EES GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 |
| title_short |
Granite genesis: in-situ melting and crustal evolution |
| ausleihindikator_str_mv |
23:s 60 65:- 120 120:g 370 |
| rolewithnormlink_str_mv |
@@689@@(DE-588)4451364-1 @@689@@(DE-588)4158036-9 @@689@@(DE-588)4132750-0 @@689@@(DE-588)4157153-8 @@689@@(DE-588)4020740-7 |
| remote_bool |
true |
| GND_str_mv |
Kontinent / Erdkruste Kontinentalkruste Kontinentale Kruste Kontinentale Erdkruste Granitische Schmelze Granit Gesteinsentstehung Petrogenese Gesteinsbildung Gesteinsbeschreibung Petrografie Petrographie Petrologie Gesteinskunde |
| GND_txt_mv |
Kontinent / Erdkruste Kontinentalkruste Kontinentale Kruste Kontinentale Erdkruste Granitische Schmelze Granit Gesteinsentstehung Petrogenese Gesteinsbildung Gesteinsbeschreibung Petrografie Petrographie Petrologie Gesteinskunde |
| GND_txtF_mv |
Kontinent / Erdkruste Kontinentalkruste Kontinentale Kruste Kontinentale Erdkruste Granitische Schmelze Granit Gesteinsentstehung Petrogenese Gesteinsbildung Gesteinsbeschreibung Petrografie Petrographie Petrologie Gesteinskunde |
| doi_str |
10.1007/978-1-4020-5891-2 |
| callnumber-a |
QE462.G7 |
| up_date |
2024-07-21T20:58:38.832Z |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a22002652 4500</leader><controlfield tag="001">55011985X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240226132524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">071122s2007 ne |||||o 00| ||eng c</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9781402058912</subfield><subfield code="9">978-1-4020-5891-2</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-1-4020-5891-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)55011985X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBV55011985X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)315762962</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)978-1-4020-5891-2</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-NL</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE462.G7</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">552.3</subfield><subfield code="2">22</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.26</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.36</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chen, Guo-Neng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Granite genesis: in-situ melting and crustal evolution</subfield><subfield code="c">edited by Guo-Neng Chen, Rodney Grapes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Dordrecht</subfield><subfield code="b">Springer Science+Business Media B.V</subfield><subfield code="c">2007</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">v.: digital</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Includes bibliographical references and index</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology</subfield></datafield><datafield tag="530" ind1=" " ind2=" "><subfield code="a">Electronic reproduction; Available via World Wide Web</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="a">Online-Ausg.</subfield><subfield code="f">Springer eBook Collection. Earth and Environmental Science</subfield><subfield code="n">Electronic reproduction; Available via World Wide Web</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geochemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Physical geography</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="D">s</subfield><subfield code="0">(DE-588)4451364-1</subfield><subfield code="0">(DE-627)227154967</subfield><subfield code="0">(DE-576)212575198</subfield><subfield code="a">Kontinentale Erdkruste</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="D">s</subfield><subfield code="0">(DE-588)4158036-9</subfield><subfield code="0">(DE-627)105496138</subfield><subfield code="0">(DE-576)209839082</subfield><subfield code="a">Granitische Schmelze</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="2"><subfield code="D">s</subfield><subfield code="0">(DE-588)4132750-0</subfield><subfield code="0">(DE-627)105685321</subfield><subfield code="0">(DE-576)209638192</subfield><subfield code="a">Granit</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="3"><subfield code="D">s</subfield><subfield code="0">(DE-588)4157153-8</subfield><subfield code="0">(DE-627)104130911</subfield><subfield code="0">(DE-576)209832223</subfield><subfield code="a">Gesteinsbildung</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="4"><subfield code="D">s</subfield><subfield code="0">(DE-588)4020740-7</subfield><subfield code="0">(DE-627)106316915</subfield><subfield code="0">(DE-576)208934626</subfield><subfield code="a">Gesteinskunde</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2=" "><subfield code="5">(DE-627)</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Grapes, Rodney</subfield><subfield code="4">oth</subfield></datafield><datafield tag="776" ind1="1" ind2=" "><subfield code="z">9781402058905</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.gbv.de/dms/bowker/toc/9781402058905.pdf</subfield><subfield code="m">V:DE-601</subfield><subfield code="m">X:Bowker</subfield><subfield code="q">pdf/application</subfield><subfield code="v">2011-12-23</subfield><subfield code="x">Verlag</subfield><subfield code="y">Inhaltsverzeichnis</subfield><subfield code="3">Inhaltsverzeichnis</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield><subfield code="b">2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-830</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_1</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_KXP</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-705</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-3</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-715</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-1373</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.26</subfield><subfield code="j">Magmatische Gesteine</subfield><subfield code="0">(DE-627)10640718X</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.36</subfield><subfield code="j">Tektonik</subfield><subfield code="0">(DE-627)106407147</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">552.3</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="b">852490046</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">olr-springer</subfield><subfield code="u">i</subfield><subfield code="y">z</subfield><subfield code="z">12-12-07</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="b">4304949497</subfield><subfield code="h">SpringerLink</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="k">Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="b">1655656309</subfield><subfield code="c">03</subfield><subfield code="f">--%%--</subfield><subfield code="d">ebook</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">k3o</subfield><subfield code="z">02-01-17</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="b">1840105739</subfield><subfield code="h">OLR-ESP</subfield><subfield code="k">Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden.</subfield><subfield code="y">z</subfield><subfield code="z">13-01-19</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="b">357768481X</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">g</subfield><subfield code="j">--%%--</subfield><subfield code="h">alma</subfield><subfield code="y">z</subfield><subfield code="z">21-01-20</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="b">1845236394</subfield><subfield code="h">olr-springer</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="u">i</subfield><subfield code="y">z</subfield><subfield code="z">27-01-19</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="y">Springer EBook</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="y">Volltextzugang Campus</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="y">Volltextzugang Campus</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="r">http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="y">E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="983" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">00</subfield><subfield code="x">DE-715</subfield><subfield code="8">99</subfield><subfield code="a">ww</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="a">YH 2020</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">olr-springer</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="a">SpringerLink</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="a">OLR-SEB-ZDB-2-EES</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="a">OLR-ESP</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="a">alma</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="a">olr-springer</subfield></datafield><datafield tag="998" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="0">2007.12.12</subfield></datafield></record></collection>
|
| fulltext |
Introduction … Crustal melting : experiments and conditions … In situ melting and intracrustal convection : granite magma layers … Geological evidence for in situ melting origin of granite layers … Differentiation of magma layer : geochemical considerations … Mineralisation related to in situ granite formation … Heat source for crustal magma layers : tectonic models … Geological effects of crystallisation of a crustal granite magma layer : SE China … Material and element cycling of the continental crust and summary … Map of SE China showing provinces Results of experimental rock melting |
| _version_ |
1805223742760026112 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a22002652 4500</leader><controlfield tag="001">55011985X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240226132524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">071122s2007 ne |||||o 00| ||eng c</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9781402058912</subfield><subfield code="9">978-1-4020-5891-2</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-1-4020-5891-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)55011985X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBV55011985X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)315762962</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)978-1-4020-5891-2</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-NL</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE462.G7</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">552.3</subfield><subfield code="2">22</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.26</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.36</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chen, Guo-Neng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Granite genesis: in-situ melting and crustal evolution</subfield><subfield code="c">edited by Guo-Neng Chen, Rodney Grapes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Dordrecht</subfield><subfield code="b">Springer Science+Business Media B.V</subfield><subfield code="c">2007</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">v.: digital</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Includes bibliographical references and index</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">FM.pdf; Ch01.pdf; Ch02.pdf; Ch03.pdf; Ch04.pdf; Ch05.pdf; Ch06.pdf; Ch07.pdf; Ch08.pdf; Ch09.pdf; Refs.pdf; Appendix 1.pdf; Appendix 2.pdf; Index.pdf</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This book reviews current ideas explaining the formation of granite in terms of melting, segregation, ascent and emplacement. It introduces an alternative hypothesis that granites are endogenic in that they essentially form and remain at melting sites in the middle-upper crust under conditions of abnormally high heat flow. The book highlights results of Chinese research over the last 30 years in English for the first time.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ melting-intracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melt layer is essential for the formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and depth of erosion. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we introduce a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology</subfield></datafield><datafield tag="530" ind1=" " ind2=" "><subfield code="a">Electronic reproduction; Available via World Wide Web</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="a">Online-Ausg.</subfield><subfield code="f">Springer eBook Collection. Earth and Environmental Science</subfield><subfield code="n">Electronic reproduction; Available via World Wide Web</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geochemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Physical geography</subfield></datafield><datafield tag="650" ind1=" " ind2="0"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="D">s</subfield><subfield code="0">(DE-588)4451364-1</subfield><subfield code="0">(DE-627)227154967</subfield><subfield code="0">(DE-576)212575198</subfield><subfield code="a">Kontinentale Erdkruste</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="D">s</subfield><subfield code="0">(DE-588)4158036-9</subfield><subfield code="0">(DE-627)105496138</subfield><subfield code="0">(DE-576)209839082</subfield><subfield code="a">Granitische Schmelze</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="2"><subfield code="D">s</subfield><subfield code="0">(DE-588)4132750-0</subfield><subfield code="0">(DE-627)105685321</subfield><subfield code="0">(DE-576)209638192</subfield><subfield code="a">Granit</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="3"><subfield code="D">s</subfield><subfield code="0">(DE-588)4157153-8</subfield><subfield code="0">(DE-627)104130911</subfield><subfield code="0">(DE-576)209832223</subfield><subfield code="a">Gesteinsbildung</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2="4"><subfield code="D">s</subfield><subfield code="0">(DE-588)4020740-7</subfield><subfield code="0">(DE-627)106316915</subfield><subfield code="0">(DE-576)208934626</subfield><subfield code="a">Gesteinskunde</subfield><subfield code="2">gnd</subfield></datafield><datafield tag="689" ind1="0" ind2=" "><subfield code="5">(DE-627)</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Grapes, Rodney</subfield><subfield code="4">oth</subfield></datafield><datafield tag="776" ind1="1" ind2=" "><subfield code="z">9781402058905</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.gbv.de/dms/bowker/toc/9781402058905.pdf</subfield><subfield code="m">V:DE-601</subfield><subfield code="m">X:Bowker</subfield><subfield code="q">pdf/application</subfield><subfield code="v">2011-12-23</subfield><subfield code="x">Verlag</subfield><subfield code="y">Inhaltsverzeichnis</subfield><subfield code="3">Inhaltsverzeichnis</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield><subfield code="b">2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-830</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_1</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_KXP</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-705</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-3</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-715</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-1373</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.26</subfield><subfield code="j">Magmatische Gesteine</subfield><subfield code="0">(DE-627)10640718X</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.36</subfield><subfield code="j">Tektonik</subfield><subfield code="0">(DE-627)106407147</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">552.3</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="b">852490046</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">olr-springer</subfield><subfield code="u">i</subfield><subfield code="y">z</subfield><subfield code="z">12-12-07</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="b">4304949497</subfield><subfield code="h">SpringerLink</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="k">Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="b">1655656309</subfield><subfield code="c">03</subfield><subfield code="f">--%%--</subfield><subfield code="d">ebook</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">k3o</subfield><subfield code="z">02-01-17</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="b">1840105739</subfield><subfield code="h">OLR-ESP</subfield><subfield code="k">Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden.</subfield><subfield code="y">z</subfield><subfield code="z">13-01-19</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="b">357768481X</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">g</subfield><subfield code="j">--%%--</subfield><subfield code="h">alma</subfield><subfield code="y">z</subfield><subfield code="z">21-01-20</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="b">1845236394</subfield><subfield code="h">olr-springer</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="u">i</subfield><subfield code="y">z</subfield><subfield code="z">27-01-19</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="y">Springer EBook</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="y">Volltextzugang Campus</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="y">Volltextzugang Campus</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="r">http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991014896780303501</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="y">E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich</subfield><subfield code="r">http://dx.doi.org/10.1007/978-1-4020-5891-2</subfield></datafield><datafield tag="983" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">00</subfield><subfield code="x">DE-715</subfield><subfield code="8">99</subfield><subfield code="a">ww</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">2006-06993, 2006-06996, 2006-06999, 2006-07000, 2006-07001, 2006-07003, 2006-07004, 2006-07005</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="a">YH 2020</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">olr-springer</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="a">SpringerLink</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="a">OLR-SEB-ZDB-2-EES</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="a">OLR-ESP</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">02</subfield><subfield code="x">0715</subfield><subfield code="a">alma</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="a">olr-springer</subfield></datafield><datafield tag="998" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="0">2007.12.12</subfield></datafield></record></collection>
|
| score |
7.014353 |