Crustal-scale tectonic wedging in the central Longmen Shan: Constraints on the uplift mechanism in the southeastern margin of the Tibetan Plateau
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- 作者：Renqi Lua ; c ; lurq127@sina.com" class="auth_mail" title="E-mail the corresponding author ; Dengfa Heb ; Xiwei Xua ; Bo Liuc
- 关键词：Seismic interpretation ; Tectonic wedge ; Frontal monocline belt ; Upper&ndash ; middle crust (UMC) ; Longmen Shan
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 March 2016
- 年：2016
- 卷：117
- 期：Complete
- 页码：73-81
- 全文大小：4811 K
文摘
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The frontal monocline belt of the LMS is a key to reveal the basement structures.
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The crustal-scale tectonic wedge lead to the uplifting of the LMS by 3–4 km.
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We conducted a crustal-scale tectonic wedging model of the central LMS thrust belt.
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Two different tectonic stages of the central LMS are distinguished since the Cenozoic.