Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Furen Xie"'
Publikováno v:
International Journal of Geophysics, Vol 2012 (2012)
The Ms 8.0 Wenchuan earthquake occurred along the Longmenshan Faults in China and was a great disaster. Most of the damage and casualties during the quake were concentrated along surface rupture zones: the 240-km-long Beichuan-Yingxiu Fault and the 7
Externí odkaz:
https://doaj.org/article/f73aaadd426349419eaaf828c86436e5
Autor:
Bing Li, Furen Xie, Jinshui Huang, Xiwei Xu, Qiliang Guo, Guangwei Zhang, Junshan Xu, Jianxin Wang, Dawei Jiang, Jian Wang, Lifeng Ding
Publikováno v:
Science China Earth Sciences. 65:1388-1398
The Dayi seismic gap of the Longmenshan thrust belt is located between the ruptures of the 2008 Wenchuan Earthquake and the 2013 Lushan Earthquake, with a length of about 40 ~ 60 km. So far, it has been still a heated debate on whether the Dayi seism
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8355571151e1be0e122a34dc6be1791
https://doi.org/10.5194/egusphere-egu22-648
https://doi.org/10.5194/egusphere-egu22-648
Publikováno v:
Quaternary International. 532:146-156
The Yushu fault is a mainly left-lateral strike slip fault with some normal component within the Ganzi-Yushu fault system in central-eastern Tibetan Plateau. In 2010, the catastrophic Yushu Ms 7.1 earthquake occurred along this fault, causing approxi
Publikováno v:
Acta Geologica Sinica - English Edition. 91:443-454
Publikováno v:
Soil Dynamics and Earthquake Engineering. 84:70-82
Seismic hazards in the Ordos Block and its periphery were estimated based on 500 years of intensity observations. Firstly, historical intensity observations were collected, the completeness of the earthquake catalog was tested, and aftershocks were d
Autor:
Karsten Reiter, Xiaofeng Cui, Oliver Heidbach, Mark D. Zoback, Birgit Müller, Friedemann Wenzel, John Reinecker, Moritz Ziegler, Furen Xie, Mary-Lou Zoback, Karl Fuchs, Mark Tingay, Mojtaba Rajabi
Publikováno v:
Tectonophysics
Knowledge of the present-day crustal in-situ stress field is a key for the understanding of geodynamic processes such as global plate tectonics and earthquakes. It is also essential for the management of geo-reservoirs and underground storage sites f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f066851da1aa10c05c804a1e956865c7
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3489894_3/component/file_5006087/3489894.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_3489894_3/component/file_5006087/3489894.pdf
Publikováno v:
Geomorphology. 239:127-141
The Yushu segment of the Ganzi–Yushu fault system (central Tibet plateau) is mainly composed by the Yushu fault and the Batang fault. The 2010 Ms 7.1 Yushu earthquake occurred on the Yushu fault, causing huge loss of lives and widespread damages to
Publikováno v:
Tectonophysics. 653:52-67
The late Quaternary activity of Yushu segment is poorly understood compared with other segments within Ganzi–Yushu Fault system. We focused on the Batang Fault, a major branch fault of the Yushu segment. Interpretation of remote sensing images and