Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan
Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are chara...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ishihara, Shunso [verfasserIn] Sasaki, Akira [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|
| Erschienen: |
Oxford, UK: Blackwell Publishing Ltd ; 1994 |
|---|
| Schlagwörter: |
|---|
| Umfang: |
Online-Ressource |
|---|
| Reproduktion: |
2006 ; Blackwell Publishing Journal Backfiles 1879-2005 |
|---|---|
| Übergeordnetes Werk: |
In: The island arc - Oxford [u.a.] : Wiley-Blackwell, 1992, 3(1994), 2, Seite 0 |
| Übergeordnetes Werk: |
volume:3 ; year:1994 ; number:2 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1111/j.1440-1738.1994.tb00100.x |
|---|
| Katalog-ID: |
NLEJ239499239 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | NLEJ239499239 | ||
| 003 | DE-627 | ||
| 005 | 20210707090011.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 120426s1994 xx |||||o 00| ||und c | ||
| 024 | 7 | |a 10.1111/j.1440-1738.1994.tb00100.x |2 doi | |
| 035 | |a (DE-627)NLEJ239499239 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 100 | 1 | |a Ishihara, Shunso |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| 264 | 1 | |a Oxford, UK |b Blackwell Publishing Ltd |c 1994 | |
| 300 | |a Online-Ressource | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. | ||
| 533 | |d 2006 |f Blackwell Publishing Journal Backfiles 1879-2005 |7 |2006|||||||||| | ||
| 650 | 4 | |a back-are magmatism | |
| 700 | 1 | |a Sasaki, Akira |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i In |t The island arc |d Oxford [u.a.] : Wiley-Blackwell, 1992 |g 3(1994), 2, Seite 0 |h Online-Ressource |w (DE-627)NLEJ24392609X |w (DE-600)2020960-5 |x 1440-1738 |7 nnns |
| 773 | 1 | 8 | |g volume:3 |g year:1994 |g number:2 |g pages:0 |
| 856 | 4 | 0 | |u http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x |q text/html |x Verlag |z Deutschlandweit zugänglich |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a ZDB-1-DJB | ||
| 912 | |a GBV_NL_ARTICLE | ||
| 951 | |a AR | ||
| 952 | |d 3 |j 1994 |e 2 |h 0 | ||
| author_variant |
s i si a s as |
|---|---|
| matchkey_str |
article:14401738:1994----::ufrstpchrceitcoltcnzioeeoisthac |
| hierarchy_sort_str |
1994 |
| publishDate |
1994 |
| allfields |
10.1111/j.1440-1738.1994.tb00100.x doi (DE-627)NLEJ239499239 DE-627 ger DE-627 rakwb Ishihara, Shunso verfasserin aut Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| back-are magmatism Sasaki, Akira verfasserin aut In The island arc Oxford [u.a.] : Wiley-Blackwell, 1992 3(1994), 2, Seite 0 Online-Ressource (DE-627)NLEJ24392609X (DE-600)2020960-5 1440-1738 nnns volume:3 year:1994 number:2 pages:0 http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 3 1994 2 0 |
| spelling |
10.1111/j.1440-1738.1994.tb00100.x doi (DE-627)NLEJ239499239 DE-627 ger DE-627 rakwb Ishihara, Shunso verfasserin aut Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| back-are magmatism Sasaki, Akira verfasserin aut In The island arc Oxford [u.a.] : Wiley-Blackwell, 1992 3(1994), 2, Seite 0 Online-Ressource (DE-627)NLEJ24392609X (DE-600)2020960-5 1440-1738 nnns volume:3 year:1994 number:2 pages:0 http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 3 1994 2 0 |
| allfields_unstemmed |
10.1111/j.1440-1738.1994.tb00100.x doi (DE-627)NLEJ239499239 DE-627 ger DE-627 rakwb Ishihara, Shunso verfasserin aut Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| back-are magmatism Sasaki, Akira verfasserin aut In The island arc Oxford [u.a.] : Wiley-Blackwell, 1992 3(1994), 2, Seite 0 Online-Ressource (DE-627)NLEJ24392609X (DE-600)2020960-5 1440-1738 nnns volume:3 year:1994 number:2 pages:0 http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 3 1994 2 0 |
| allfieldsGer |
10.1111/j.1440-1738.1994.tb00100.x doi (DE-627)NLEJ239499239 DE-627 ger DE-627 rakwb Ishihara, Shunso verfasserin aut Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| back-are magmatism Sasaki, Akira verfasserin aut In The island arc Oxford [u.a.] : Wiley-Blackwell, 1992 3(1994), 2, Seite 0 Online-Ressource (DE-627)NLEJ24392609X (DE-600)2020960-5 1440-1738 nnns volume:3 year:1994 number:2 pages:0 http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 3 1994 2 0 |
| allfieldsSound |
10.1111/j.1440-1738.1994.tb00100.x doi (DE-627)NLEJ239499239 DE-627 ger DE-627 rakwb Ishihara, Shunso verfasserin aut Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan Oxford, UK Blackwell Publishing Ltd 1994 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| back-are magmatism Sasaki, Akira verfasserin aut In The island arc Oxford [u.a.] : Wiley-Blackwell, 1992 3(1994), 2, Seite 0 Online-Ressource (DE-627)NLEJ24392609X (DE-600)2020960-5 1440-1738 nnns volume:3 year:1994 number:2 pages:0 http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 3 1994 2 0 |
| source |
In The island arc 3(1994), 2, Seite 0 volume:3 year:1994 number:2 pages:0 |
| sourceStr |
In The island arc 3(1994), 2, Seite 0 volume:3 year:1994 number:2 pages:0 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
back-are magmatism |
| isfreeaccess_bool |
false |
| container_title |
The island arc |
| authorswithroles_txt_mv |
Ishihara, Shunso @@aut@@ Sasaki, Akira @@aut@@ |
| publishDateDaySort_date |
1994-01-01T00:00:00Z |
| hierarchy_top_id |
NLEJ24392609X |
| id |
NLEJ239499239 |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ239499239</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707090011.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120426s1994 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1440-1738.1994.tb00100.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ239499239</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="100" ind1="1" ind2=" "><subfield code="a">Ishihara, Shunso</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1994</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2006</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2006||||||||||</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">back-are magmatism</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sasaki, Akira</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">The island arc</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1992</subfield><subfield code="g">3(1994), 2, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ24392609X</subfield><subfield code="w">(DE-600)2020960-5</subfield><subfield code="x">1440-1738</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:3</subfield><subfield code="g">year:1994</subfield><subfield code="g">number:2</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">3</subfield><subfield code="j">1994</subfield><subfield code="e">2</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| series2 |
Blackwell Publishing Journal Backfiles 1879-2005 |
| author |
Ishihara, Shunso |
| spellingShingle |
Ishihara, Shunso misc back-are magmatism Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| authorStr |
Ishihara, Shunso |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)NLEJ24392609X |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut |
| collection |
NL |
| publishPlace |
Oxford, UK |
| remote_str |
true |
| illustrated |
Not Illustrated |
| issn |
1440-1738 |
| topic_title |
Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan back-are magmatism |
| publisher |
Blackwell Publishing Ltd |
| publisherStr |
Blackwell Publishing Ltd |
| topic |
misc back-are magmatism |
| topic_unstemmed |
misc back-are magmatism |
| topic_browse |
misc back-are magmatism |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| hierarchy_parent_title |
The island arc |
| hierarchy_parent_id |
NLEJ24392609X |
| hierarchy_top_title |
The island arc |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)NLEJ24392609X (DE-600)2020960-5 |
| title |
Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| ctrlnum |
(DE-627)NLEJ239499239 |
| title_full |
Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| author_sort |
Ishihara, Shunso |
| journal |
The island arc |
| journalStr |
The island arc |
| isOA_bool |
false |
| recordtype |
marc |
| publishDateSort |
1994 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Ishihara, Shunso Sasaki, Akira |
| container_volume |
3 |
| physical |
Online-Ressource |
| format_se |
Elektronische Aufsätze |
| author-letter |
Ishihara, Shunso |
| doi_str_mv |
10.1111/j.1440-1738.1994.tb00100.x |
| author2-role |
verfasserin |
| title_sort |
sulfur isotopic characteristics of late cenozoic ore deposits at the arc junction of hokkaido, japan |
| title_auth |
Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| abstract |
Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. |
| abstractGer |
Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. |
| abstract_unstemmed |
Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido. |
| collection_details |
GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE |
| container_issue |
2 |
| title_short |
Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan |
| url |
http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x |
| remote_bool |
true |
| author2 |
Sasaki, Akira |
| author2Str |
Sasaki, Akira |
| ppnlink |
NLEJ24392609X |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1111/j.1440-1738.1994.tb00100.x |
| up_date |
2024-07-06T07:37:34.237Z |
| _version_ |
1803814388879065088 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ239499239</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707090011.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120426s1994 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1440-1738.1994.tb00100.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ239499239</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="100" ind1="1" ind2=" "><subfield code="a">Ishihara, Shunso</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Sulfur isotopic characteristics of late Cenozoic ore deposits at the arc junction of Hokkaido, Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1994</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Sulfide minerals of late Cenozoic vein-type deposits of southwest Hokkaido and Kuril Islands yielded δ34CDT S values of 2 to 8 permil, which are typical green-tuff values of magnetite-series igneous terrane. Sulfides of the Kitami district of northeast Hokkaido, on the other hand, are characterized by negative δ34SCDT values, ranging from 0 to - 7 permil. This unique value among ore deposits in the late Cenozoic back-arc terranes in the Japanese Islands is considered to have resulted from extraction of 32S enriched sulfur from the basement rocks, because of well-developed N-S fracturing in the basement, which is characteristic of the axial belt and Kitami district of Hokkaido.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2006</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2006||||||||||</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">back-are magmatism</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sasaki, Akira</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">The island arc</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1992</subfield><subfield code="g">3(1994), 2, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ24392609X</subfield><subfield code="w">(DE-600)2020960-5</subfield><subfield code="x">1440-1738</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:3</subfield><subfield code="g">year:1994</subfield><subfield code="g">number:2</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1440-1738.1994.tb00100.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">3</subfield><subfield code="j">1994</subfield><subfield code="e">2</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.398945 |