Carboniferous-Permian tectonic evolution and sedimentation of the Turpan-Hami Basin, NW China: Implications for the closure of the Paleo-Asian Ocean
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- 作者：Suhua Jianga ; b ; jiangsuh@163.com" class="auth_mail" title="E-mail the corresponding author ; Sanzhong Lia ; b ; Ian D. Somervillec ; Jianping Leia ; b ; Hongying Yanga ; b
- 关键词：Turpan-Hami Basin ; Carboniferous&ndash ; Permian ; Tectonic evolution ; Sedimentary characteristics ; Structural interpretation
- 刊名：Journal of Asian Earth Sciences
- 出版年：2015
- 出版时间：1 December 2015
- 年：2015
- 卷：113
- 期：part_P2
- 页码：644-655
- 全文大小：7379 K
文摘
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Tectonic evolution is mainly characterized by stretching and uplifting.
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The closure processes of the Paleo-Asian Ocean is in Middle Permian.
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Carboniferous is the target layer for further exploration.