Early Mesozoic southward subduction history of the Mongol-Okhotsk oceanic plate: Evidence from geochronology and geochemistry of Early Mesozoic intrusive rocks in the Erguna Massif, NE China
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- 作者：Jie Tanga ; tangjie11@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Wen-Liang Xua ; b ; xuwl@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Feng Wanga ; fengwang10@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Shuo Zhaoa ; zhaoshuo12@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Wei Wanga ; wangwei11@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author
- 关键词：Erguna Massif ; Early Mesozoic magmatism ; Geochronology ; Geochemistry ; Mongol&ndash ; Okhotsk tectonic regime
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：March 2016
- 年：2016
- 卷：31
- 期：Complete
- 页码：218-240
- 全文大小：4244 K
文摘
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Early Mesozoic magmatisms in the Erguna Massif can be subdivided into four stages.
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Early Mesozoic magmatisms formed mainly in an active continental margin setting.
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The Mongol–Okhotsk oceanic plate was subducted southward during Early Mesozoic.