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Chun Fan

Researcher at China University of Geosciences (Beijing)

Publications -  8
Citations -  292

Chun Fan is an academic researcher from China University of Geosciences (Beijing). The author has contributed to research in topics: Plateau & Shear zone. The author has an hindex of 4, co-authored 8 publications receiving 233 citations. Previous affiliations of Chun Fan include Chinese Academy of Sciences.

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Slip rate gradients along the eastern Kunlun fault

TL;DR: In this paper, the authors present new slip rate determinations using millennial-scale geomorphic markers from sites along the easternmost segment of the Kunlun fault in north central Tibet.
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Late Cenozoic river system reorganization and its origin within the Qilian Shan, NE Tibet

TL;DR: In this article, the authors present evidence that the left-lateral movement of the Haiyuan Fault (one of the largest active strike-slip faults within the Tibetan Plateau since ~13-8-Ma) created a series of NW-trending linear thrust-fold belts, aligned in an en echelon pattern along the trace of the fault.
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Young, active conjugate strike–slip deformation in West Sichuan: evidence for the stress–strain pattern of the southeastern Tibetan Plateau

TL;DR: In this paper, the authors define two sets of young, active strike-slip faults within the northern part of the Chuan-Dian crustal fragment that lie within the SE Tibetan Plateau.
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Structural control on the topography of the Laji–Jishi and Riyue Shan belts in the NE margin of the Tibetan plateau: Facilitation of the headward propagation of the Yellow River system

TL;DR: In this article, the authors show that the variation in deformation along this mountain belt formed two structural saddles with relative low elevation in late Cenozoic time, through which the Yellow and Yaoshui Rivers cut into the plateau and drained a series of Tertiary basins.
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GPS Strain Rate and Seismic Activity Before the Ludian Earthquake (Ms 6.5), Northeast Yunnan, China: New Implications for Eastward Chuan-Dian Block Extrusion

TL;DR: In this paper, the authors characterized E-W shortening crustal deformation using GPS measurements and an earthquake focal mechanism solution to estimate conditions before the 6.5 Ludian earthquake of 3 August 2014 (16:30, UTC+8).