H
Haisheng Yi
Researcher at Chengdu University of Technology
Publications - 20
Citations - 1068
Haisheng Yi is an academic researcher from Chengdu University of Technology. The author has contributed to research in topics: Sedimentary rock & Plateau. The author has an hindex of 8, co-authored 14 publications receiving 885 citations.
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Journal ArticleDOI
Constraints on the early uplift history of the Tibetan Plateau
Chengshan Wang,Xixi Zhao,Zhifei Liu,Peter C. Lippert,Stephan A. Graham,Robert S. Coe,Haisheng Yi,Lidong Zhu,Shun Liu,Yalin Li +9 more
TL;DR: Geologic and geophysical data from north-central Tibet are presented, including magnetostratigraphy, sedimentology, paleocurrent measurements, and 40Ar/39Ar and fission-track studies, to show that the central plateau was elevated by 40 Ma ago.
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Tectonic and sedimentary evolution of basins in the northeast of Qinghai-Tibet Plateau and their implication for the northward growth of the Plateau
TL;DR: In this paper, the authors studied the evolution of the Qinghai-Tibet Plateau and its associated basins, finding that the basins began as strike-slip basins and evolved into intermontane basins.
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Magnetostratigraphy of Tertiary sediments from the Hoh Xil Basin: implications for the Cenozoic tectonic history of the Tibetan Plateau
TL;DR: In this article, the authors conducted an integrated palaeomagnetic and stratigraphic study on a 5452.8 m thick sedimentary sequence of the Hoh Xil Basin in northern Qinghai-Tibet Plateau to obtain a chronostratigraphic framework for these sediments.
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Tertiary crustal shortening and peneplanation in the Hoh Xil region: implications for the tectonic history of the northern Tibetan Plateau
TL;DR: The Fenghuoshan and overlying Yaxicuo groups span the Eocene-Early Oligocene stratigraphically, and have been dated by magnetostratigraphy as 56-30 Ma old as mentioned in this paper.
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Evolution and Mass Accumulation of the Cenozoic Hoh Xil Basin, Northern Tibet
TL;DR: In this article, the authors reconstruct the depositional history and estimates the mass of sediments stored in the Hoh Xil basin, northern Tibet, the largest Cenozoic sedimentary basin in the hinterland of the Tibetan Plateau.