Generating early continental crust

Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentative...
Ausführliche Beschreibung

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Autor*in:	Wellhäuser, Alexander - 1988- [verfasserIn] Wörner, Gerhard [akademischer betreuerIn] Rushmer, Tracy [akademischer betreuerIn] Kley, Jonas [akademischer betreuerIn] Pack, Andreas [akademischer betreuerIn] Schmidt, Burkhard [akademischer betreuerIn] Turner, Simon [akademischer betreuerIn]
Hochschulschrift:	Dissertation ; Georg-August-Universität Göttingen ; 2020

Format:	E-Book
Sprache:	Englisch

Erschienen:	Göttingen: 2020

Formangabe:	Hochschulschrift

Umfang:	1 Online-Ressource ; Illustrationen, Diagramme

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Wellhäuser, Alexander, 1988 -: Generating early continental crust - Göttingen, 2020

Links:	Link aufrufen Volltext Volltext Link aufrufen

DOI / URN:	urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4

Katalog-ID:	172416337X

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520			\|a Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme...
520			\|a Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo...
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Indexfelder

author_variant	a w aw
matchkey_str	wellhuseralexanderwrnergerhardrushmertra:2020----:eeaigalcni
hierarchy_sort_str	2020
bklnumber	38.35
publishDate	2020
allfields	1213520525 DE-101 urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 urn 21.11130/00-1735-0000-0005-140E-6 hdl (DE-627)172416337X (DE-599)KXP172416337X DE-627 ger DE-627 rda eng XA-DE-NI 910 ; 550 22 552 DE-101 550 DE-101 38.35 bkl Wellhäuser, Alexander 1988- verfasserin (DE-588)1227889763 (DE-627)1749088231 aut Generating early continental crust submitted by Alexander Wellhäuser ; Reviewer: Prof. Dr. Gerhard Wörner, Second Reviewer: A/Prof. Dr. Tracy Rushmer, Further members of the Examination Board: Prof. Dr. Jonas Kley, Prof. Dr. Andreas Pack, Dr. Burkhard Schmidt, Prof. Dr. Simon Turner Göttingen 2020 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2020 Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Wörner, Gerhard akademischer betreuerin dgs Rushmer, Tracy akademischer betreuerin dgs Kley, Jonas akademischer betreuerin dgs Pack, Andreas akademischer betreuerin dgs Schmidt, Burkhard akademischer betreuerin dgs Turner, Simon akademischer betreuerin dgs Göttingen (DE-588)4021477-1 (DE-627)106313819 (DE-576)20893815X uvp Erscheint auch als Druck-Ausgabe Wellhäuser, Alexander, 1988 - Generating early continental crust Göttingen, 2020 v, 140 Seiten (DE-627)1724163388 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 Resolving-System kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 Resolving-System kostenfrei Volltext https://d-nb.info/1213520525/34 2020-08-05 Langzeitarchivierung Nationalbibliothek GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER 38.35 Endogene Geologie: Allgemeines (DE-627)106407155 BO 045F 910 ; 550 045F 552 20 01 0084 3736455933 x 08-08-20 21 01 0046 3736483597 z 08-08-20 22 01 0018 3736536917 SUBolrd xu 08-08-20 23 01 0830 373657939X olr-d x 08-08-20 30 01 0104 3736612761 z 08-08-20 40 01 0007 372286223X ediss xsn 10-07-20 60 01 0705 3736694288 OLRD z 08-08-20 63 01 3401 3736730756 ORD x 08-08-20 70 01 0089 3736768109 zdo 08-08-20 105 01 0841 373704676X z 08-08-20 110 01 3110 3736796072 x 08-08-20 132 01 0959 3736831935 OLR-DISS x 08-08-20 151 01 0546 3736859201 OLR-ODISS z 08-08-20 161 01 0960 3736892268 ORD z 08-08-20 293 01 3293 3736994869 ORD z 08-08-20 370 01 4370 3737008167 x 08-08-20 2403 01 DE-LFER 373636041X 00 --%%-- --%%-- n --%%-- l01 07-08-20 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 01 0007 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 LF Volltext 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 00 DE-7 00 (DE-627)62504584X V 000 Geologische Wissenschaften 40 00 DE-7 01 (DE-627)62504617X VAE 500 Geotektonische Entwicklung der Erdkruste {Tektonik} 40 00 DE-7 02 (DE-627)625046307 VAE 860 Festlandkerne {Tektonik} 40 00 DE-7 03 (DE-627)625054113 VJB 310 Geochemie der kontinentalen Kruste 40 00 DE-7 04 (DE-627)625048415 VDD 000 Archaikum 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-08-08:01:17:44
spelling	1213520525 DE-101 urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 urn 21.11130/00-1735-0000-0005-140E-6 hdl (DE-627)172416337X (DE-599)KXP172416337X DE-627 ger DE-627 rda eng XA-DE-NI 910 ; 550 22 552 DE-101 550 DE-101 38.35 bkl Wellhäuser, Alexander 1988- verfasserin (DE-588)1227889763 (DE-627)1749088231 aut Generating early continental crust submitted by Alexander Wellhäuser ; Reviewer: Prof. Dr. Gerhard Wörner, Second Reviewer: A/Prof. Dr. Tracy Rushmer, Further members of the Examination Board: Prof. Dr. Jonas Kley, Prof. Dr. Andreas Pack, Dr. Burkhard Schmidt, Prof. Dr. Simon Turner Göttingen 2020 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2020 Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Wörner, Gerhard akademischer betreuerin dgs Rushmer, Tracy akademischer betreuerin dgs Kley, Jonas akademischer betreuerin dgs Pack, Andreas akademischer betreuerin dgs Schmidt, Burkhard akademischer betreuerin dgs Turner, Simon akademischer betreuerin dgs Göttingen (DE-588)4021477-1 (DE-627)106313819 (DE-576)20893815X uvp Erscheint auch als Druck-Ausgabe Wellhäuser, Alexander, 1988 - Generating early continental crust Göttingen, 2020 v, 140 Seiten (DE-627)1724163388 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 Resolving-System kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 Resolving-System kostenfrei Volltext https://d-nb.info/1213520525/34 2020-08-05 Langzeitarchivierung Nationalbibliothek GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER 38.35 Endogene Geologie: Allgemeines (DE-627)106407155 BO 045F 910 ; 550 045F 552 20 01 0084 3736455933 x 08-08-20 21 01 0046 3736483597 z 08-08-20 22 01 0018 3736536917 SUBolrd xu 08-08-20 23 01 0830 373657939X olr-d x 08-08-20 30 01 0104 3736612761 z 08-08-20 40 01 0007 372286223X ediss xsn 10-07-20 60 01 0705 3736694288 OLRD z 08-08-20 63 01 3401 3736730756 ORD x 08-08-20 70 01 0089 3736768109 zdo 08-08-20 105 01 0841 373704676X z 08-08-20 110 01 3110 3736796072 x 08-08-20 132 01 0959 3736831935 OLR-DISS x 08-08-20 151 01 0546 3736859201 OLR-ODISS z 08-08-20 161 01 0960 3736892268 ORD z 08-08-20 293 01 3293 3736994869 ORD z 08-08-20 370 01 4370 3737008167 x 08-08-20 2403 01 DE-LFER 373636041X 00 --%%-- --%%-- n --%%-- l01 07-08-20 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 01 0007 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 LF Volltext 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 00 DE-7 00 (DE-627)62504584X V 000 Geologische Wissenschaften 40 00 DE-7 01 (DE-627)62504617X VAE 500 Geotektonische Entwicklung der Erdkruste {Tektonik} 40 00 DE-7 02 (DE-627)625046307 VAE 860 Festlandkerne {Tektonik} 40 00 DE-7 03 (DE-627)625054113 VJB 310 Geochemie der kontinentalen Kruste 40 00 DE-7 04 (DE-627)625048415 VDD 000 Archaikum 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-08-08:01:17:44
allfields_unstemmed	1213520525 DE-101 urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 urn 21.11130/00-1735-0000-0005-140E-6 hdl (DE-627)172416337X (DE-599)KXP172416337X DE-627 ger DE-627 rda eng XA-DE-NI 910 ; 550 22 552 DE-101 550 DE-101 38.35 bkl Wellhäuser, Alexander 1988- verfasserin (DE-588)1227889763 (DE-627)1749088231 aut Generating early continental crust submitted by Alexander Wellhäuser ; Reviewer: Prof. Dr. Gerhard Wörner, Second Reviewer: A/Prof. Dr. Tracy Rushmer, Further members of the Examination Board: Prof. Dr. Jonas Kley, Prof. Dr. Andreas Pack, Dr. Burkhard Schmidt, Prof. Dr. Simon Turner Göttingen 2020 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2020 Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Wörner, Gerhard akademischer betreuerin dgs Rushmer, Tracy akademischer betreuerin dgs Kley, Jonas akademischer betreuerin dgs Pack, Andreas akademischer betreuerin dgs Schmidt, Burkhard akademischer betreuerin dgs Turner, Simon akademischer betreuerin dgs Göttingen (DE-588)4021477-1 (DE-627)106313819 (DE-576)20893815X uvp Erscheint auch als Druck-Ausgabe Wellhäuser, Alexander, 1988 - Generating early continental crust Göttingen, 2020 v, 140 Seiten (DE-627)1724163388 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 Resolving-System kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 Resolving-System kostenfrei Volltext https://d-nb.info/1213520525/34 2020-08-05 Langzeitarchivierung Nationalbibliothek GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER 38.35 Endogene Geologie: Allgemeines (DE-627)106407155 BO 045F 910 ; 550 045F 552 20 01 0084 3736455933 x 08-08-20 21 01 0046 3736483597 z 08-08-20 22 01 0018 3736536917 SUBolrd xu 08-08-20 23 01 0830 373657939X olr-d x 08-08-20 30 01 0104 3736612761 z 08-08-20 40 01 0007 372286223X ediss xsn 10-07-20 60 01 0705 3736694288 OLRD z 08-08-20 63 01 3401 3736730756 ORD x 08-08-20 70 01 0089 3736768109 zdo 08-08-20 105 01 0841 373704676X z 08-08-20 110 01 3110 3736796072 x 08-08-20 132 01 0959 3736831935 OLR-DISS x 08-08-20 151 01 0546 3736859201 OLR-ODISS z 08-08-20 161 01 0960 3736892268 ORD z 08-08-20 293 01 3293 3736994869 ORD z 08-08-20 370 01 4370 3737008167 x 08-08-20 2403 01 DE-LFER 373636041X 00 --%%-- --%%-- n --%%-- l01 07-08-20 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 01 0007 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 LF Volltext 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 00 DE-7 00 (DE-627)62504584X V 000 Geologische Wissenschaften 40 00 DE-7 01 (DE-627)62504617X VAE 500 Geotektonische Entwicklung der Erdkruste {Tektonik} 40 00 DE-7 02 (DE-627)625046307 VAE 860 Festlandkerne {Tektonik} 40 00 DE-7 03 (DE-627)625054113 VJB 310 Geochemie der kontinentalen Kruste 40 00 DE-7 04 (DE-627)625048415 VDD 000 Archaikum 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-08-08:01:17:44
allfieldsGer	1213520525 DE-101 urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 urn 21.11130/00-1735-0000-0005-140E-6 hdl (DE-627)172416337X (DE-599)KXP172416337X DE-627 ger DE-627 rda eng XA-DE-NI 910 ; 550 22 552 DE-101 550 DE-101 38.35 bkl Wellhäuser, Alexander 1988- verfasserin (DE-588)1227889763 (DE-627)1749088231 aut Generating early continental crust submitted by Alexander Wellhäuser ; Reviewer: Prof. Dr. Gerhard Wörner, Second Reviewer: A/Prof. Dr. Tracy Rushmer, Further members of the Examination Board: Prof. Dr. Jonas Kley, Prof. Dr. Andreas Pack, Dr. Burkhard Schmidt, Prof. Dr. Simon Turner Göttingen 2020 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2020 Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Wörner, Gerhard akademischer betreuerin dgs Rushmer, Tracy akademischer betreuerin dgs Kley, Jonas akademischer betreuerin dgs Pack, Andreas akademischer betreuerin dgs Schmidt, Burkhard akademischer betreuerin dgs Turner, Simon akademischer betreuerin dgs Göttingen (DE-588)4021477-1 (DE-627)106313819 (DE-576)20893815X uvp Erscheint auch als Druck-Ausgabe Wellhäuser, Alexander, 1988 - Generating early continental crust Göttingen, 2020 v, 140 Seiten (DE-627)1724163388 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 Resolving-System kostenfrei Volltext http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 Resolving-System kostenfrei Volltext https://d-nb.info/1213520525/34 2020-08-05 Langzeitarchivierung Nationalbibliothek GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER 38.35 Endogene Geologie: Allgemeines (DE-627)106407155 BO 045F 910 ; 550 045F 552 20 01 0084 3736455933 x 08-08-20 21 01 0046 3736483597 z 08-08-20 22 01 0018 3736536917 SUBolrd xu 08-08-20 23 01 0830 373657939X olr-d x 08-08-20 30 01 0104 3736612761 z 08-08-20 40 01 0007 372286223X ediss xsn 10-07-20 60 01 0705 3736694288 OLRD z 08-08-20 63 01 3401 3736730756 ORD x 08-08-20 70 01 0089 3736768109 zdo 08-08-20 105 01 0841 373704676X z 08-08-20 110 01 3110 3736796072 x 08-08-20 132 01 0959 3736831935 OLR-DISS x 08-08-20 151 01 0546 3736859201 OLR-ODISS z 08-08-20 161 01 0960 3736892268 ORD z 08-08-20 293 01 3293 3736994869 ORD z 08-08-20 370 01 4370 3737008167 x 08-08-20 2403 01 DE-LFER 373636041X 00 --%%-- --%%-- n --%%-- l01 07-08-20 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 01 0007 http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 LF Volltext 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 2403 01 DE-LFER http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 40 00 DE-7 00 (DE-627)62504584X V 000 Geologische Wissenschaften 40 00 DE-7 01 (DE-627)62504617X VAE 500 Geotektonische Entwicklung der Erdkruste {Tektonik} 40 00 DE-7 02 (DE-627)625046307 VAE 860 Festlandkerne {Tektonik} 40 00 DE-7 03 (DE-627)625054113 VJB 310 Geochemie der kontinentalen Kruste 40 00 DE-7 04 (DE-627)625048415 VDD 000 Archaikum 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2020-08-08:01:17:44
allfieldsSound	1213520525 DE-101 urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 urn 21.11130/00-1735-0000-0005-140E-6 hdl (DE-627)172416337X (DE-599)KXP172416337X DE-627 ger DE-627 rda eng XA-DE-NI 910 ; 550 22 552 DE-101 550 DE-101 38.35 bkl Wellhäuser, Alexander 1988- verfasserin (DE-588)1227889763 (DE-627)1749088231 aut Generating early continental crust submitted by Alexander Wellhäuser ; Reviewer: Prof. Dr. Gerhard Wörner, Second Reviewer: A/Prof. Dr. Tracy Rushmer, Further members of the Examination Board: Prof. Dr. Jonas Kley, Prof. Dr. Andreas Pack, Dr. Burkhard Schmidt, Prof. Dr. Simon Turner Göttingen 2020 1 Online-Ressource Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Georg-August-Universität Göttingen 2020 Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo... 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language	English
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hochschulschrift_txt_mv	Dissertation Georg-August-Universität Göttingen 2020
dewey-raw	910 ; 550
isfreeaccess_bool	true
authorswithroles_txt_mv	Wellhäuser, Alexander @@aut@@ Wörner, Gerhard @@dgs@@ Rushmer, Tracy @@dgs@@ Kley, Jonas @@dgs@@ Pack, Andreas @@dgs@@ Schmidt, Burkhard @@dgs@@ Turner, Simon @@dgs@@
publishDateDaySort_date	2020-01-01T00:00:00Z
dewey-sort	3910 3550
id	172416337X
genre_facet	Hochschulschrift
language_de	englisch
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title_sort	generating early continental crust
title_auth	Generating early continental crust
abstract	Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo...
abstractGer	Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo...
abstract_unstemmed	Archaische Kratone sind Relikte der geodynamischen Prozesse, die das Antlitz der Erde in ihrer frühen Entwicklung prägten. Sie bestehen aus Plutoniten felsischer Zusammensetzung, umschlossen von gefalteten vulkanisch und sedimentär geprägten Abfolgen. Jedoch bilden diese Gesteine kein repräsentatives Archiv der krustalen Entwicklung, sondern sind einzelne Fragmente, räumlich und zeitlich voneinander getrennt. Je älter die geologischen Formationen, desto uneindeutiger ist ihre Entstehungsgeschichte, nicht zuletzt aufgrund von zum Teil mehrfacher metamorpher Überprägung. Vor allem die Zusamme... Archean cratons are the products of geodynamic processes governing the evolution of the early Earth. They comprise felsic granitoids enclosed by folded volcano-sedimentary successions. However, these rocks may not be representative archives but rather accidental fragments in time and space. The further back the rock record reaches in time, the more ambiguous it becomes, not least because of multiple subsequent overprinting events. The composition of Archean granitoids is distinctly different to post-Archean felsic rocks that are associated with modern continental crust forming processes. Mo...
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title_short	Generating early continental crust
url	http://hdl.handle.net/21.11130/00-1735-0000-0005-140E-6 http://nbn-resolving.org/urn:nbn:de:gbv:7-21.11130/00-1735-0000-0005-140E-6-4 https://d-nb.info/1213520525/34
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remote_bool	true
author2	Wörner, Gerhard Rushmer, Tracy Kley, Jonas Pack, Andreas Schmidt, Burkhard Turner, Simon
author2Str	Wörner, Gerhard Rushmer, Tracy Kley, Jonas Pack, Andreas Schmidt, Burkhard Turner, Simon
ppnlink	1724163388
GND_str_mv	Wellhäuser, Alexander Hochschulschrift Gotingē Gettingen Goddinga Gottinga Goettinga Stadt Göttingen Götingen Gutingi Gottingen Gothinga Gëttingen Göttingen
GND_txt_mv	Wellhäuser, Alexander Hochschulschrift Gotingē Gettingen Goddinga Gottinga Goettinga Stadt Göttingen Götingen Gutingi Gottingen Gothinga Gëttingen Göttingen
GND_txtF_mv	Wellhäuser, Alexander Hochschulschrift Gotingē Gettingen Goddinga Gottinga Goettinga Stadt Göttingen Götingen Gutingi Gottingen Gothinga Gëttingen Göttingen
mediatype_str_mv	c
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up_date	2024-07-04T09:43:21.492Z
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Generating early continental crust

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Zugang & Verfügbarkeit

Vorhandene Bände

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