Zobrazeno 1 - 10
of 96
pro vyhledávání: '"Liangshu Wang"'
Autor:
Zhouchuan Huang, Cong Ji, Hanting Wu, Yutong Shi, Jiaqi Geng, Mijian Xu, Cunrui Han, Mingjie Xu, Liangshu Wang
Publikováno v:
地球与行星物理论评, Vol 52, Iss 3, Pp 291-307 (2021)
The uplift of the Tibetan Plateau in the Cenozoic has changed the tectonics of the whole Asia and affected the climate and environment significantly. However, the mechanism of the plateau uplift and expansion is still in debate. The southeastern marg
Externí odkaz:
https://doaj.org/article/884707be5e984fa1a1115cfd16301732
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 3, Pp n/a-n/a (2020)
Abstract Structural heterogeneities in subduction zones can affect slip behaviors of the megathrust faults and the generation of intraslab earthquakes. In this work we study the 3‐D seismic structures (Vp, Vs, and Poisson's ratio) in and around the
Externí odkaz:
https://doaj.org/article/e70827ff60314e54a206933a11074fd5
Autor:
Chao Li, Shengli Wang, Yongxiang Li, Yan Chen, Hugh Sinclair, Dongtao Wei, Delong Ma, Huayu Lu, Xianyan Wang, Liangshu Wang
Publikováno v:
Li, C, Wang, S, Li, Y, Chen, Y, Sinclair, H, Wei, D, Ma, D, Lu, H, Wang, X & Wang, L 2022, ' Growth of the Tian Shan drives migration of the conglomerate-sandstone transition in the southern Junggar foreland basin ', Geophysical Research Letters, vol. 49, no. 4, e2021GL097545 . https://doi.org/10.1029/2021GL097545
The conglomerate-sandstone transition (CST) preserved in foreland basins records the stratigraphic equivalent of the gravel to sand transition (GST) which migrates in response to shortening in steady state orogen-foreland basin systems. Two seismic p
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:10292-10308
Publikováno v:
Earth and Planetary Science Letters. 598:117837
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:8890-8907
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:7052-7066
Publikováno v:
Geophysical Journal International. 218:2066-2078
SUMMARYFocal mechanism solutions (FMSs) reflect the stress field underground directly. They provide essential clue for crustal deformations and therefore improve our understanding of tectonic uplift and expansion of the Tibetan Plateau. In this study
Publikováno v:
Journal of Asian Earth Sciences. 176:88-104
Since the Late Cenozoic, the central-southern Longmen Shan (LMS) region is characterized by a two-decollement thrust-fold system with a localized upper evaporite weaker layer just beneath the Sichuan Basin and the lower stronger decollement beneath t
Publikováno v:
Journal of Asian Earth Sciences. 172:101-114
The modern Tian Shan formed due to the India-Eurasia collision. Uplift of the Tian Shan is recorded notably by the sedimentary sequences and subsidence history of the coupling foreland basins. We analyzed a 353-km-long seismic profile and logging dat