Late Paleozoic subduction and collision processes during the amalgamation of the Central Asian Orogenic Belt along the South Tianshan suture zone
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- 作者：Yigui Hana ; Guochun Zhaoa ; gzhao@hkucc.hku.hk" class="auth_mail" title="E-mail the corresponding author ; Min Suna ; Paul R. Eizenhö ; fera ; b ; Wenzhu Houa ; Xiaoran Zhanga ; Qian Liua ; Bo Wangc ; Dongxing Liuc ; Bing Xuc
- 关键词：Tarim ; Tianshan ; Subduction orogeny ; Collision orogeny ; Detrital zircon ; Mantle plume
- 刊名：Lithos
- 出版年：2016
- 出版时间：March 2016
- 年：2016
- 卷：246-247
- 期：Complete
- 页码：1-12
- 全文大小：2934 K
文摘
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The South Tianshan Ocean was northward subducted in the Early Carboniferous.
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The Central Tianshan–Yili Block and Tarim Craton collided in the Late Carboniferous.
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Foreland basin was starved of orogenic detritus throughout Carboniferous–Permian time.
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A mantle plume-modified collisional orogeny has been proposed.
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