Tectonic attribution of the Langshan area in western Inner Mongolia and implications for the Neoarchean-Paleoproterozoic evolution of the Western North China Craton: Evidence from LA-ICP-MS zircon U-Pb dating of the Langshan basement
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- 作者：Zeng-Zhen Wang ; Bao-Fu Han ; bfhan@pku.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Li-Xia Feng ; Bo Liu ; Bo Zheng ; Ling-Jie Kong
- 关键词：LA-ICP-MS ; Neoarchean&ndash ; Paleoproterozoic ; Langshan basement ; Alxa Block ; North China Craton
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 September 2016
- 年：2016
- 卷：261
- 期：Complete
- 页码：278-295
- 全文大小：5966 K
文摘
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The Langshan area may be subdivided into the Main and Southern Langshan.
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The Main Langshan basements were mainly formed during Neoarchean–Paleoproterozoic.
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The Main Langshan probably belongs to the Yinshan Block in northern NCC.
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The late Paleoproterozoic and Neoproterozoic basement rocks exist in the Southern Langshan.
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The Southern Langshan probably belongs to the Alxa Block.