Solonker ophiolite in Inner Mongolia, China: A late Permian continental margin-type ophiolite
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- 作者：Zhi-wen Luoa ; Bei Xua ; ; Guan-zhong Shib ; Pan Zhaoa ; M. Faurec ; Yan Chenc
- 关键词：Solonker ophiolite ; Solonker zone ; Late Permian ; Continental margin ; Extension
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 September 2016
- 年：2016
- 卷：261
- 期：Complete
- 页码：72-91
- 全文大小：5046 K
文摘
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The Solonker ophiolite formed at ca. 260 Ma.
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The Solonker ophiolite is a CM-type body that formed during early stages of opening of a small ocean basin rather than remnants of Paleo-Asian Ocean.
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The evolution of the Solonker zone in Permian is characterized by intra-continental extension.