Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere
Sikhote-Alin and Sakhalin are located in the Russian Far East flank of the northernmost part of the Sea of Japan. Magmatism in this region preceded, was concurrent with, and continued after the exten-sion and sea-floor spreading (25–18Ma) that formed the Sea of Japan. Among the Sikhote-Alin and Sakh...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.596.5653 2023-05-15T18:08:48+02:00 Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere Satoshi Okamura Richard J. Arculus Yuri A. Martynov The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.5653 http://petrology.oxfordjournals.org/content/46/2/221.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.5653 http://petrology.oxfordjournals.org/content/46/2/221.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://petrology.oxfordjournals.org/content/46/2/221.full.pdf KEY WORDS north-eastern Eurasian margin Sikhote-Alin–Sakhal text 2003 ftciteseerx 2016-01-08T13:45:47Z Sikhote-Alin and Sakhalin are located in the Russian Far East flank of the northernmost part of the Sea of Japan. Magmatism in this region preceded, was concurrent with, and continued after the exten-sion and sea-floor spreading (25–18Ma) that formed the Sea of Japan. Among the Sikhote-Alin and Sakhalin volcanic suites, Eocene–Oligocene (55–24Ma) lavas are characterized by greater large ion lithophile element and rare earth element enrichments compared with Early–Mid-Miocene (23–15Ma) tholeiites, and also show a depletion in high field strength elements (HFSE). The geochemical characteristics of the Eocene–Oligocene and Early– Mid-Miocene basalts are consistent with migration of the locus of magma generation beneath the Sikhote-Alin and Sakhalin areas from subduction-modified lithospheric mantle into mid-ocean ridge basalt (MORB)-source asthenosphere as spreading in the Sea of Japan progressed. Mid-Miocene–Pliocene (14–5Ma) lavas, erupted fol- Text Sakhalin Unknown Sion ENVELOPE(13.758,13.758,66.844,66.844) |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
topic |
KEY WORDS north-eastern Eurasian margin Sikhote-Alin–Sakhal |
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KEY WORDS north-eastern Eurasian margin Sikhote-Alin–Sakhal Satoshi Okamura Richard J. Arculus Yuri A. Martynov Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
topic_facet |
KEY WORDS north-eastern Eurasian margin Sikhote-Alin–Sakhal |
description |
Sikhote-Alin and Sakhalin are located in the Russian Far East flank of the northernmost part of the Sea of Japan. Magmatism in this region preceded, was concurrent with, and continued after the exten-sion and sea-floor spreading (25–18Ma) that formed the Sea of Japan. Among the Sikhote-Alin and Sakhalin volcanic suites, Eocene–Oligocene (55–24Ma) lavas are characterized by greater large ion lithophile element and rare earth element enrichments compared with Early–Mid-Miocene (23–15Ma) tholeiites, and also show a depletion in high field strength elements (HFSE). The geochemical characteristics of the Eocene–Oligocene and Early– Mid-Miocene basalts are consistent with migration of the locus of magma generation beneath the Sikhote-Alin and Sakhalin areas from subduction-modified lithospheric mantle into mid-ocean ridge basalt (MORB)-source asthenosphere as spreading in the Sea of Japan progressed. Mid-Miocene–Pliocene (14–5Ma) lavas, erupted fol- |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Satoshi Okamura Richard J. Arculus Yuri A. Martynov |
author_facet |
Satoshi Okamura Richard J. Arculus Yuri A. Martynov |
author_sort |
Satoshi Okamura |
title |
Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
title_short |
Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
title_full |
Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
title_fullStr |
Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
title_full_unstemmed |
Cenozoic Magmatism of the North-Eastern Eurasian Margin: The Role of Lithosphere Versus Asthenosphere |
title_sort |
cenozoic magmatism of the north-eastern eurasian margin: the role of lithosphere versus asthenosphere |
publishDate |
2003 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.5653 http://petrology.oxfordjournals.org/content/46/2/221.full.pdf |
long_lat |
ENVELOPE(13.758,13.758,66.844,66.844) |
geographic |
Sion |
geographic_facet |
Sion |
genre |
Sakhalin |
genre_facet |
Sakhalin |
op_source |
http://petrology.oxfordjournals.org/content/46/2/221.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.5653 http://petrology.oxfordjournals.org/content/46/2/221.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766181126052773888 |