Výsledky vyhledávání - "Xiongnan Huang"

Akademický článek

Late Quaternary faulting and paleoearthquakes along the northern section of the Bayanhaote fault and their implications for regional seismotectonics

Autor: Guihua Chen, Zhongwu Li, Xiongnan Huang

Publikováno v: Frontiers in Earth Science, Vol 10 (2022)

Analysis of the late Quaternary activity and paleoseismicity of the Bayanhaote fault is critical because it is part of the frontier of the propagating Tibetan Plateau and the boundary between the Alxa and Ordos blocks, and the development of a region

Externí odkaz: https://doaj.org/article/705236ca3ce04aa283f8c38aa87a6439

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Akademický článek

Re-Evaluating the Surface Rupture and Slip Distribution of the AD 1609 M7 1/4 Hongyapu Earthquake Along the Northern Margin of the Qilian Shan, NW China: Implications for Thrust Fault Rupture Segmentation

Autor: Xiongnan Huang, Xiaoping Yang, Haibo Yang, Zongkai Hu, Ling Zhang

Publikováno v: Frontiers in Earth Science, Vol 9 (2021)

The Hexi Corridor is located beyond the northeastern edge of the Tibetan Plateau, and it is bounded by a series of active thrusts along the northern margin of the Qilian Shan and the southern piedmont of the Longshou Shan. Historically, five destruct

Externí odkaz: https://doaj.org/article/b8068837a15c4f0886863a7579c0151e

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Akademický článek

China Active Faults Database and its web system.

Autor: Xiyan Wu, Xiwei Xu, Guihua Yu, Junjie Ren, Xiaoping Yang, Guihua Chen, Chong Xu, Keping Du, Xiongnan Huang, Haibo Yang, Kang Li, Haijian Hao

Publikováno v: Earth System Science Data Discussions; 6/6/2023, p1-31, 31p

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Late Miocene to Quaternary Development of the Jiujing Basin, Southern Beishan Block, China: Implications for the Kinematics and Timing of Crustal Reactivation North of Tibet

Autor: Haibo Yang, Dickson Cunningham, Zongkai Hu, Xiaoping Yang, Huili Yang, Xiongnan Huang

Publikováno v: Lithosphere. 2021

We present results from a multidisciplinary investigation of the Jiujing fault (JJF) system and adjacent Jiujing Basin in the southern Beishan block, western China. Structural and geomorphological fieldwork involving fault and landform investigations

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::65be7149f3d39b0827a018114892da9e
https://doi.org/10.2113/2021/6670365

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Active fold deformation and crustal shortening rates of the Qilian Shan Foreland Thrust Belt, NE Tibet, since the Late Pleistocene

Autor: Xiaoping Yang, Haibo Yang, Ning Zhang, Xiongnan Huang, Weiliang Huang, Huiping Zhang

Publikováno v: Tectonophysics. :84-100

Quantification of crustal shortening rates across foreland fold-and-thrust belts is essential for evaluating how convergence is accommodated throughout the orogenic belt and analyzing seismic hazard in neighboring cities. In this study, we focused on

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::82231ebd692a467a639a6dd4a7595ad5
https://doi.org/10.1016/j.tecto.2018.05.019

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New constraints on slip rates of the Fodongmiao-Hongyazi fault in the Northern Qilian Shan, NE Tibet, from the 10Be exposure dating of offset terraces

Autor: Xiongnan Huang, Weiliang Huang, Haibo Yang, Ling Zhang, An Li, Xiaoping Yang

Publikováno v: Journal of Asian Earth Sciences. 151:131-147

The Fodongmo-Hongyazi fault (FHF) is a major thrust of Northeastern Tibet, bounding the Qilian Shan. It accommodates crustal shortening across this region and has produced a strong historical earthquake. Until now the slip rate has been poorly constr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3619c26fdd94870a0fe8c4eb4379fbc0
https://doi.org/10.1016/j.jseaes.2017.10.034

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Holocene paleoeseismology of the Fodongmiao-Hongyazi Fault along the Northern Tibetan margin (Western China) and implication to intraplate earthquake rupturing pattern

Autor: Haibo Yang, Ling Zhang, Zongkai Hu, Huili Yang, Xiaoping Yang, Xiongnan Huang

Publikováno v: Tectonophysics. 808:228812

The margins of the Tibetan Plateau are the most recent evolving part of the orogen, where distributed fault systems accumulate intraplate crustal deformation induced by the Indo-Asian collision, and many great earthquakes occur. Understanding the pal

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::073952d701e9e3d365e961dce79000a1
https://doi.org/10.1016/j.tecto.2021.228812

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