Notice, Smithsonian Terms of This dissertation explores the uses for data collected at broadband seismic stations to investigate source process of large strike-slip earthquakes and crust and upper mantle structure within active continental tectonic settings. Four major earthquakes of M s >7.0 occurred in the Tibetan Plateau during the last decade. The dynamics of the earthquake rupture process are closely related to fault zone properties which the authors have intensively investigated by various observations in the field as well as by laboratory experiments. Found inside â Page 19... Fu B, Guo J, Zeng Q, Dang G, He W, Zhao Y (2002) Co-seismic strike-slip and rupture length produced by the 2001 Ms 8.1 Central Kunlun earthquake. Found inside â Page 151These include the Mw 7.8 Kunlun Mountain Pass earthquake (KMPE) of 14 November 2001, the Mw 7.9 Wenchuan, Sichuan, earthquake of 12 May 2008, and the Mw 6.9 ... With a magnitude of 7.8 Mw it was the most powerful earthquake in China for 5 decades. This earthquake was associated with the longest surface rupture ever recorded on land, ~450 km. The rupture propagated to the east via an extensional stepover before following the main strand of the Kunlun fault. The region of co-seismic deformation (i.e. It occurred on 14 November, 2001, on the Kunlun Fault north of Tibet. The 2001 Kunlun earthquake also known as the 2001 Kokoxili earthquake, occurred on 14 November 2001 at 09:26 UTC (17:26 local time), with an epicenter near Kokoxili, close to the border between Qinghai and Xinjiang in a remote mountainous region. The rupture length and maximum displacement are the largest among the co-seismic surface rupture . Download . Found inside â Page 59... similar to those produced during the 2001 Mw 7.8 Kunlun earthquake along the typical right-lateral strikeâslip Kunlun Fault (Lin et al. 2004) (Figs. The rupture zone may be divided into four segments based on the geological structures, tectonic landform features, spatial . This is an audio version of the Wikipedia Article:https://en.wikipedia.org/wiki/2001_Kunlun_earthquake00:00:44 1 Tectonic setting00:01:12 2 Earthquake00:02:4. [5], An analysis of the propagation speed indicates that the rupture propagated at a normal velocity along the original segment, but increased in velocity to above the S-wave velocity after the jump across the extensional stepover and continued at that speed until propagation stopped. The 2001 Kunlun earthquake also known as the 2001 Kokoxili earthquake, occurred on 14 November 2001 at 09:26 UTC (17:26 local time), with an epicenter near Kokoxili, close to the border between Qinghai and Xinjiang in a remote mountainous region. Earthquakes similar to or like 2001 Kunlun earthquake. Found inside â Page 2359However, before the Kunlun Earthquake (M 8.1, Nov. 14, 2001) we did not find an anomaly in the LURR contour map near the epicenter. Further study shows that ... Retrieved 30 January 2019. Med en styrke på 7,8 M w var det det kraftigste jordskælv i Kina i 5 årtier. Received 2008 May 15; in original form 2008 March 8 SUMMARY Non-volcanic tremor (NVT) is an extended-duration and non-impulsive . The rupture zone may be divided into four segments based on the geological structures, tectonic landform features, spatial . With a magnitude of 7.8 M w it was the most powerful earthquake in China for 5 decades. With a magnitude of 7.8 Mw it was the most powerful. Some damage was reported at the construction site for the Qingzang railway (Qinghai-Tibet railway)[3] and along the Qinghai-Tibet highway. Found inside â Page 51OBSERVED EVIDENCE FOR CRACK FUSION FROM THE NOVEMBER 14, 2001 KUNLUN MOUNTAIN PASS EARTHQUAKE XU LI-SHENGâ and CHEN YUN-TAIâ Institute of Geophysics, ... rupture process for this earthquake, in order to obtain the maximum rupture speed attained. The inset shows the regional location of the earthquake. About Cookies, including instructions on how to turn off cookies if you wish to do so. Made available by U.S. Department of Energy Office of Scientific and Technical Information . 2010-08-25 00:00:00 1. Den 2001 Kunlun jordskælv også kendt som Kokoxili jordskælv 2001, fandt sted den 14. november 2001 kl 09:26 UTC (17:26 lokal tid), med en epicenter nær Kokoxili, tæt på grænsen mellem Qinghai og Xinjiang i en fjern bjergområde. They were the 2001 M s 8.1 Kunlun Mountains (Hoh Xil) earthquake in Qinghai, the 2008 M s 7.3 Yutian earthquake in Xinjiang, the 2008 M s 8.0 Wenchuan earthquake in Sichuan, and the 2010 M s 7.1 Yushu earthquake in Qinghai. No casualties were reported, presumably due to the very low . The 2001 Mw7.8 Kokoxili earthquake ruptured the western segment of the Kunlun fault and produced a ~420-km-long coseismic surface rupture, as well as significant postseismic deformation. Found inside â Page 169... for the Kunlun (China) earthquake of 14 November 2001, MW 1â4 7.8, and the corresponding theoretical directivity function (broken line) for a source of ... With a magnitude of 7.8 M w it was the most powerful earthquake in China for 5 decades. The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Found insideNo instrument can tell when and where an earthquake will happen. So instead of trying to guess, itâs better to be prepared. This book will detail what will happen when an Earthquake happens. Open this book today! [1], "Preliminary report on the Ms 8.1 Kokoxili (Qinghai, China) earthquake of 14 November 2001", "High-Resolution Satellite Imagery Mapping of the Surface Rupture and Slip Distribution of the Mw _7.8, 14 November 2001 Kokoxili Earthquake, Kunlun Fault, Northern Tibet, China", "The 14 November 2001, Mw 7.8 Kokoxili earthquake in northern Tibet (Qinghai Province, China)", "Spatial distribution of the surface rupture zone associated with the 2001 Ms 8.1 Central Kunlun earthquake, northern Tibet, revealed by satellite remote sensing data", "Observation of Long Supershear Rupture During the Magnitude 8.1 Kunlunshan Earthquake", "The Aftershock Signature of Supershear Earthquakes", China International Search and Rescue Team, https://en.wikipedia.org/w/index.php?title=2001_Kunlun_earthquake&oldid=1036260876, Creative Commons Attribution-ShareAlike License, This page was last edited on 30 July 2021, at 12:42. 1174 M. Antolik, R. E. Abercrombie, and G. Ekstro¨m 90 o92 94 96o 36o 50 km Qaidam Basin Kunlun Range HSL 3 2 1 Figure 1. The 2001 Kunlun earthquake also known as the 2001 Kokoxili earthquake, occurred on 14 November 2001 at 09:26 UTC (17:26 local time), with an epicenter near Kokoxili, close to the border between Qinghai and Xinjiang in a remote mountainous region. The 2001 Kunlun earthquake also known as the 2001 Kokoxili earthquake, occurred on 14 November 2001 at 09:26 UTC (17:26 local time), with an epicenter near Kokoxili, close to the border between Qinghai and Xinjiang in a remote mountainous region. 18.10.2020 (a) Shuttle Radar Topography Mission (SRTM, 90-m resolution) color-shaded relief map showing the topographic features and distribution of the major active faults in the … 2002; Fig. Field investigations allow us to constrain the coseismic surface rupture zone of ∼400 km with a strike slip up to 16.3 m associated with the 2001 M w 7.8 Central Kunlun earthquake that occurred along one of the western segments of the Kunlun fault, northern Tibet. International Journal of Remote Sensing. ↑ Liu, J. G.; Haselwimmer, C. E. (2006). No casualties were reported, presumably due to the very low .
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