Apatite fission track evidence for the Cretaceous-Cenozoic cooling history of the Qilian Shan (NW China) and for stepwise northeastward growth of the northeastern Tibetan Plateau since early Eocene
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- 作者：Bangshen Qia ; b ; qibangshen@126.com" class="auth_mail" title="E-mail the corresponding author ; Daogong Hua ; Xiaoxiao Yangc ; Yaoling Zhanga ; Chengxuan Tana ; b ; Peng Zhanga ; b ; Chengjun Fenga ; b
- 关键词：Fission track analysis ; Apatite ; Qilian Shan ; Stepwise growth ; Cretaceous ; Cenozoic
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 July 2016
- 年：2016
- 卷：124
- 期：Complete
- 页码：28-41
- 全文大小：8933 K
文摘
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AFT data from the Qilian Shan indicate stepwise northeastward growth of the northeastern Tibetan Plateau since the early Eocene, corresponding to India–Eurasia collision.
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Rapid cooling during Cretaceous corresponds to the collision of the Lhasa block with the Eurasian.
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Rapid cooling since early Eocene in the South Qilian Shan corresponds to India–Eurasia collision.
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The study results shed light on the tectonic evolution of the Qilian Shan.