Late Permian-Early Triassic traps of the Kuznetsk Basin, Russia: Geochemistry and petrogenesis in respect to an extension of the Siberian Large Igneous Province
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- 作者：Tatyana V. Svetlitskayaa ; svt@igm.nsc.ru" class="auth_mail" title="E-mail the corresponding author ; Peter A. Nevolkoa ; b
- 关键词：Mafic lavas ; Geochemistry ; Petrogenesis ; Siberian Large Igneous Province ; Kuznetsk Basin ; Russian
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：39
- 期：Complete
- 页码：57-76
- 全文大小：4451 K
文摘
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The Kuznetsk lavas originated from low-degree partial melting of spinel lherzolite.
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The Kuznetsk lavas are characterized by both OIB-like and subduction-like signatures.
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The Kuznetsk Basin is a part of the Siberian Large Igneous Province.