| Genesis of the Cenozoic Sodic Alkaline Basalt in the Xiahe–Tongren Area of the Northeastern Tibetan Plateau and its Continental Dynamic Implications |
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| 作者姓名： | LAI Shaocong |
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| 作者单位： | State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, Shaanxi, China |
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| 基金项目： | This work was supported by the National Natural Science Foundation of China (grant No. 41072052). |
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| 摘 要： | 正Objective The Cenozoic Indo-Asian collision caused significant crustal shortening and plateau uplift in the central Tibet.The extrusion tectonic model has been widely accepted to explain the strike-slip faults around the Tibetan Plateau.Previous studies indicate that the lower crust flow is the
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Genesis of the Cenozoic Sodic Alkaline Basalt in the Xiahe–Tongren Area of the Northeastern Tibetan Plateau and its Continental Dynamic Implications |
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| Authors: | LAI Shaocong |
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| Institution: | State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Shaanxi, China |
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