Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Shitan Nie"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 9, Pp n/a-n/a (2024)
Abstract Understanding how the Miocene N–S‐trending rifts on the southern Tibetan Plateau formed is crucial for understanding the evolution of the plateau. Most competing models suggest that all the rifts developed uniformly, but there are differ
Externí odkaz:
https://doaj.org/article/625fa71f2e454c968927aa4327d2ecc9
Autor:
Gaochun Wang, Xiaobo Tian, Yibing Li, Tao Xu, Bo Wan, Yi Chen, Shitan Nie, Xusong Yang, Sicheng Zuo, Jianli Zhang
Publikováno v:
Earthquake Research Advances, Vol 3, Iss 3, Pp 100233- (2023)
The relationship of the crustal contact between the Indian and Eurasian plates is a key issue in understanding crustal thickening and the subduction of the Indian lithosphere beneath the Qinghai-Tibetan Plateau. Across the middle of the Yarlung-Zangb
Externí odkaz:
https://doaj.org/article/bebbe4e73e3c44a2b5ab0cc4e3498eee
Publikováno v:
Journal of Geophysical Research: Solid Earth. 128
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e61350a97d3372e5af9f35c7cb919ad7
https://doi.org/10.1029/2022jb025747
https://doi.org/10.1029/2022jb025747
Autor:
Tian Cui, Wei-wei Ding, Wei Li, Xiao-dong Wei, Yangfan Deng, Ping Tan, Yun Chen, Shitan Nie, Jiwen Teng, Shuai Xue, Zhiming Bai
Publikováno v:
Solid Earth Sciences, Vol 4, Iss 3, Pp 85-91 (2019)
The East China Continental Margin (ECCM) is an exemplified natural laboratory not only for studying the origin and evolution of trench-arc-basin system, but also for investigating the deformation mechanism within continent and its margins. For a bett
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06815e98a4f928d9a38380adda5dfeb8
http://www.sciencedirect.com/science/article/pii/S2451912X19300157
http://www.sciencedirect.com/science/article/pii/S2451912X19300157
Autor:
Shitan Nie, Ping Tan
Publikováno v:
Physics of the Earth and Planetary Interiors. 321:106801
Crustal anisotropy beneath a dense broadband seismic array across the Longmenshan fault belt is measured based on P-to-S converted phases from the Moho and an intra-crustal interface. The crustal thickness and the average Vp/Vs values are also estima
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9d093d278225dd5ef7e3db58e3de870
https://doi.org/10.1016/j.pepi.2021.106801
https://doi.org/10.1016/j.pepi.2021.106801
Autor:
Beibei Zhou, Gaochun Wang, Rui Gao, Xiaobo Tian, Guiping Yu, Gaohua Zhu, Zhen Liu, Shitan Nie, Zhenbo Wu, Ping Tan, Xiao Xu
Publikováno v:
Earth and Planetary Science Letters. 480:33-41
An east–west trending, high-density seismic array was deployed along the eastern margin of the Tibetan Plateau to investigate its eastward expansion. The 160 km long array spans the Ruoergai basin, Minjiang fault, Minshan Mountains, Tazang fault, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c53c1f24e44c951f692d382b102d6a66
https://doi.org/10.1016/j.epsl.2017.09.048
https://doi.org/10.1016/j.epsl.2017.09.048
Publikováno v:
Journal of Asian Earth Sciences. 206:104629
A mass of lithospheric shortening occurred beneath the Tibetan Plateau due to the collision between the Indian and Eurasian plates. The extrusion of the upper crust beneath the Tibetan Plateau has been widely accepted, but whether the lithospheric ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::945f699d91769db9f7f1e0793d63ce8e
https://doi.org/10.1016/j.jseaes.2020.104629
https://doi.org/10.1016/j.jseaes.2020.104629
Autor:
Zhi Wei, Yaohui Duan, Zhiming Bai, Xi Zhang, Gaohua Zhu, Wei Li, Zhenbo Wu, Zhen Liu, Jiwen Teng, Minling Wang, Xiaofeng Liang, Tao Xu, Xi Guo, Xiaobo Tian, Beibei Zhou, Gaochun Wang, Chenglong Wu, Yun Chen, Xiaopeng Zhou, Guiping Yu, Shitan Nie, Minghui Zhang
Publikováno v:
Seismological Research Letters. 87:864-873
The tectonic processes that formed the Tibetan plateau have been a significant topic in earth science, but images of the subducting Indian continental lithosphere (ICL) are still not clear enough to reveal detailed continental collision processes. Se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9316e0f93c9628c10bd45e6a9fb1d787
https://doi.org/10.1785/0220150243
https://doi.org/10.1785/0220150243
Publikováno v:
Tectonophysics. 788:228499
The north-south convergence between the Indian and Eurasian continents since Cenozoic has produced the Tibetan plateau, and east-west extension structures have also developed since late Cenozoic. Whether these extensional structures are limited to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea4492aa8cda7a27d336030156ddd69c
https://doi.org/10.1016/j.tecto.2020.228499
https://doi.org/10.1016/j.tecto.2020.228499
Autor:
Gaohua Zhu, Yun Chen, Xiaobo Tian, Hongshuang Zhang, Beibei Zhou, Zhen Liu, Chenglong Wu, Ping Tan, Wei Li, Guiping Yu, Sicheng Zuo, Xiaofeng Liang, Shitan Nie, Xiaohui Yuan, Gaochun Wang
Publikováno v:
Earth and Planetary Science Letters
The convergence between the Indian and Eurasian plates has produced the thick crust and uplifted the Tibetan plateau since about 50 Ma. However, the deformation of the mantle lithosphere is still a puzzle. The geometry of the subducting Indian mantle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f900c89231bfc5f0646139fa3bf8335e
https://doi.org/10.1016/j.epsl.2019.115954
https://doi.org/10.1016/j.epsl.2019.115954