Middle Jurassic oceanic island igneous rocks of the Raohe accretionary complex, northeastern China: Petrogenesis and tectonic implications
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- 作者：Zhi-Hui Wang wangzh12@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Wen-Chun Ge ; gewenchun@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Hao Yang yanghao12@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Yan-Long Zhang zhangyanlong@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Jun-Hui Bi biying2746@126.com" class="auth_mail" title="E-mail the corresponding author ; De-Xin Tian 2272450096@qq.com" class="auth_mail" title="E-mail the corresponding author ; Wen-Liang Xu xuwl@jlu.edu.con" class="auth_mail" title="E-mail the corresponding author
- 关键词：Raohe accretionary complex ; Middle Jurassic ; Paleo-Pacific Ocean ; Ocean island basalts ; Major and trace element geochemistry ; Nadanhada Range
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：1 November 2015
- 年：2015
- 卷：111
- 期：Complete
- 页码：120-137
- 全文大小：6067 K
文摘
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The igneous rocks of the Raohe accretionary complex formed at 169–167 Ma.
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The intrusive rocks were derived from a similar mantle source with the OIBs.
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They were formed by low degree of melting (<5%) in the garnet stability field.
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They formed in a plume-related intra-plate oceanic setting.
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