Yuqi Hao
China Earthquake Administration
15 Papers
2 Citations
Yuqi Hao is an academic researcher from China Earthquake Administration. The author has contributed to research in topics: Geology & Cenozoic. The author has an hindex of 4, co-authored 9 publications.
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Papers
Miocene Range Growth Along the Altyn Tagh Fault: Insights From Apatite Fission Track and (U-Th)/He Thermochronometry in the Western Danghenan Shan, China
Jingxing Yu,Jingxing Yu,Dewen Zheng,Dewen Zheng,Jianzhang Pang,Yizhou Wang,Matthew Fox,Pieter Vermeesch,Chaopeng Li,Lin Xiao,Yuqi Hao,Ying Wang +11 more
TL;DR: In this paper, the authors report new 14-16 Ma apatite fission track (AFT) and 9-11 Ma AAFT/AHe data in the western Danghenan Shan, north Tibet.
Late Oligocene tectonic uplift of the East Kunlun Shan: expansion of the northeastern Tibetan Plateau
Chaopeng Li,Dewen Zheng,Renjie Zhou,Jingxing Yu,Yizhou Wang,Jianzhang Pang,Ying Wang,Yuqi Hao,Youjuan Li +8 more
TL;DR: In this paper, the authors focus on the East Kunlun Shan (EKLS), where the timing of Cenozoic deformation remains controversial, and collect seven apatite (U•Th)/He samples around a tilted erosion surface in the middle segment of the EKLS.
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Constraints of new apatite fission-track ages on the tectonic pattern and geomorphic development of the northern margin of the Tibetan Plateau
Jianzhang Pang,Jingxing Yu,Jingxing Yu,Dewen Zheng,Dewen Zheng,Yizhou Wang,Huiping Zhang,Chaopeng Li,Weitao Wang,Yuqi Hao +9 more
TL;DR: In this article, the authors collected 11 apatite fission-track samples along an elevation transect to the south of Jiayuguan to unravel the cooling history and erosion variation of the northern margin of western section of the Qilian Shan.
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Topographic growth of the northeastern Tibetan Plateau during the middle-late Miocene: Insights from integrated provenance analysis in the NE Qaidam Basin
Chaopeng Li,Chaopeng Li,Chaopeng Li,Dewen Zheng,Renjie Zhou,Weitao Wang,Jingxing Yu,Caicai Liu,Yizhou Wang,Jianzhang Pang,Yan Ma,Yuqi Hao,Youjuan Li,Xueye Wang +13 more
TL;DR: In this article, the authors present integrated provenance data from the NE Qaidam Basin, south of the Qilian Shan, and infer that significant topographic growth occurred during the middle to late Miocene, and abruptly shifts on provenance, sedimentary facies and climate indexes in its surrounding basins.
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