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Wuheshalu Fault

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Journal Article
Journal: Lithosphere
Published: 23 May 2019
Lithosphere (2019) 11 (4): 507-523.
... section, maybe because faulting and northward propagation of the North Pamir caused northward displacement of the depocenter to north of the Wuheshalu section. * Corresponding author: hlchen@zju.edu.cn 08 07 2018 24 02 2019 11 03 2019 © 2019 The Authors 2019 Gold Open...
FIGURES | View All (8)
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Representative outcrop photographs from the <b>Wuheshalu</b> section. (A) The Pami...
Published: 23 May 2019
Figure 4. Representative outcrop photographs from the Wuheshalu section. (A) The Pamir Frontal Thrust carrying Paleogene strata over the Miocene Pakabulake Formation. (B) The lower Anjuan Formation with relatively more abundant mudstone interrupted by two small thrust faults. (C) Appearance
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Simplified late Cenozoic evolutionary model of the Pamir–South Tian Shan (S...
Published: 23 May 2019
belt also provided a minor amount of detritus to the Wuheshalu area, leading to a mixed provenance and an E-directed paleocurrent direction. (C) During deposition of the upper Atushi Formation, northward thrusting of PFT and Wuheshalu fault (WF) resulted in northward propagation of the North Pamir
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Interpretation of seismic profiles showing structures of (A) the A–A′ secti...
Published: 23 May 2019
) (modified after Wang et al., 2016 ). Locations are shown in Figure 1B . WF—Wuheshalu fault; STS—South Tian Shan. Note that the vertical scale is exaggerated.
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(A) Digital elevation model and structural interpretation of the Pamir and ...
Published: 23 May 2019
Belt; KYTS—Kashi-Yecheng Transfer System; TFF—Talas-Fergana fault; WF—Wuheshalu fault. Locations of previous detrital zircon research and magnetostratigraphic sections are shown ( Bershaw et al., 2012 ; Yang et al., 2014 , 2015 , 2017 , 2018 ; Chen et al., 2015 ; Tang et al., 2015 ; Thompson et
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The late Cenozoic stratigraphy, sample location (including samples for detr...
Published: 23 May 2019
Figure 5. The late Cenozoic stratigraphy, sample location (including samples for detrital zircon U-Pb analysis and sites for conglomerate clast counting), paleocurrent directions, and sedimentary accumulation rates of the Wuheshalu section, with its correlation to the previous late Cenozoic