Preliminary reports indicate a maximum offset of 7 meters (23 feet) in the central section of the break. Adopting these data, constrained by detail surface rupture data mea￣sured after the earthquake, we inverted the co seismic slip distribution along the seismic fault. The inset shows the epicentre of the 2001 M w 7.8 Kunlun earthquake (green star), the tremor location (red star), and the great circle ray path. Just better. Kunlun earthquake On 14 November 2001 the Central Kunlun earthquake (Ms 8.1) took place along the Sun Lake, Kusai Lake, Earthquake fissure Dongdatan and Xidatan segments of the EKF on the northeast Tibetan Plateau (Lin et al.2002; Xu et al.2002; Fissures are the most developed surface rupture style Van der Woerd et al. To install click the Add extension button. 2001 Kunlun Earthquake A Great earthquake hit the Kunlun Fault on November 14, 2001. Posted on October 22, 2020 by October 22, 2020 by Inset shows earthquake dislocations along the Kunlun fault since 1930, emphasizing the very long rupture length of the 14 November 2001 earthquake and the seismic gap along the Xidatan–Dongdatan segment (different shades are used to distinguish between over- lapping ruptures, modified from Van der Woerd et al. The quake affected the Peruvian regions of Arequipa, Moquegua and Tacna.It was the most devastating earthquake in Peru since the catastrophic 1970 Ancash earthquake and globally the largest earthquake since the 1965 Rat Islands earthquake. This fault initiates near the Bukadaban Peak (36.0 N, 90.5 E) in the west, and extends eastwards through the Hoh Sai Lake, south of the Yuzhu Peak, and terminates about 70 km east of the Kunlun Pass (35.4 N, 95.2 E). How to transfigure the Wikipedia . Tremor occurs when the Love wave displacement is to the southwest (the lateral motion direction for the CR), suggesting a simple frictional response to the driving force. The most recent earthquake on the Kunlun fault occurred on November 14, 2001. The 2001 Kunlun earthquake produced surface ruptures that total at least 410 km in length (Xu et al. The 2002 Denali Fault and 2001 Kunlun Fault Earthquakes S279 Figure 1. The 2001 Kunlun earthquake, therefore, provides us with an unusual opportunity to understand the rupture mechanism and process along a large continental strike-slip fault. Yi‐Ying Wen, Kuo‐Fong Ma, Teh‐Ru Alex Song, Walter D. Mooney, Validation of the rupture properties of the 2001 Kunlun, China (Ms= 8.1), earthquake from seismological and geological observations, Geophysical Journal International, 10.1111/j.1365-246X.2008.04063.x, 177, 2, (555-570), (2009). Kunlun earthquake (Tibetan plateau) of 14 November 2001 produced a nearly 400-kilometer-long surface rupture zone, with as much as 16.3 meters of left-lateral strike-slip along the active Kunlun fault in northern Tibet. Short‐time postseismic deformation of 2001 Ms8.1 Kunlun (China) earthquake Short‐time postseismic deformation of 2001 Ms8.1 Kunlun (China) earthquake Rundle, John B. That's it. At a magnitude of 8.1, it produced a surface break over 350 kilometers (217 miles) long. Systematical Stream Offsets Resulting from Large Earthquakes Along the Strike-Slip Kunlun Fault, Northern Tibetan Plateau: Evidence from the 2001 Mw 7.8 Kunlun Earthquake The Open Geology Journal, 2008, 2: 1-9 Aiming Lin Institute of Geosciences, Faculty of Science, Shizuoka University, Shizuoka 422-8529, Japan. INTRODUCTION On November 14, 2001, the Ms 8.1 earthquake occurred in the Tibetan Plateau in China 36.2°N, 90.9°E. In this paper, we invert the co‐seismic GPS and InSAR data for a robust finite‐fault model of the Kunlun earthquake based on a realistic fault geometry buried in a layered earth structure. The M s 8.1 Central Kunlun earthquake occurred on 14 November 2001 in the Kunlun mountain area . The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. Simplified tectonic maps of our study areas: (A) Alaska-western Canada, and (B) Himalayan-Tibetan orogen. Le Pichon,1 J. Guilbert,1 M. Valle´e,1 J. X. Dessa,2 and M. Ulziibat3 Received 22 April 2003; revised 16 June 2003; accepted 24 June 2003; published 12 August 2003. "Validation of the rupture properties of the 2001 Kunlun, China (M-s=8.1), earthquake from seismological and geological observations." 2002, 2006; Lasserre et al. The Kunlun earthquake, of moment magnitude (M w) 7.8, occurred on 14 November 2001 along the Kusai Lake–Kunlun Pass fault of the Kunlun fault system, northern Tibet (Fig. 1997). [1] We extend a model of a two-dimensional self-healing slip pulse, propagating 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. Media in category "Earthquakes of 2001" The following 8 files are in this category, out of 8 total. (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 … Wiley Online Library . [2002b]). The surface rupture generally trends N80 –85 W (Fig. The co seismic displacement field of the 2001 west of Kunlun Mountain Pass earthquake is obtained through the analysis of GPS data mea￣sured before and after the earthquake and leveling data measured in 1979 and 2002. The mole track structures appear in an angular-ridge pattern, which resembles an angular triangle-shaped frame, and in a bulge pattern forming small flat hillocks. 2002; Fig. (b) A schematic cross-section of geological features in southern Taiwan along AA' in (a). Rupture map of the Kokoxili earthquake. (2009) Wen et al. [1] On November 14, 2001, a strong earthquake occurred on the high plateau of western China. You could also do it yourself at any point in time. Farther to the north, the large intra-continental Altyn Tagh fault system also helps to accommodate this motion. Figure 2. The rupture length and maximum displacement are the largest among the co-seismic surface rupture zones reported on so far. Extensive co-seismic mole track structures have been observed along a 400-km-long surface rupture zone associated with the 2001 Ms 8.1 Central Kunlun earthquake, north Tibet. At a magnitude of 8.1, it produced a surface break over 350 kilometers (217 miles) long. 2005, 2006). Earthquake distribution 2001.png 574 × 436; 119 KB. We determine the finite-fault slip distribution of the 2001 Kunlun earthquake (Ms = 8.1) by inverting teleseismic waveforms, as constrained by geological and remote sensing field observations. 2002, 2003; Xu et al. Infrasonic imaging of the Kunlun Mountains for the great 2001 China earthquake A. 2001 Kunlun earthquake. The spatial slip distribution along the 400-km-long fault was divided into five segments in accordance with geological observations. Egepg1.jpg 418 × 312; 44 KB. Egeover2.jpg 235 × 176; 20 KB. 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. The rupture process of this event is examined by using the teleseismic body-wave data collected by IRIS-DMC stations. 2001 2001 southern Peru earthquake intesity map.jpg 612 × 720; 108 KB. Here we show clear evidence of NVT beneath the Central Range (CR) in Taiwan triggered by the 2001 M w 7.8 Kunlun earthquake in northern Tibet. 2001 Kunlun earthquake tended to follow the pre-existing palaeo-earthquake fault zone (Xu et al. 1; Lin et al., 2002, Van der Woerd et al., 2002a, Xu et al., 2002). Preliminary reports indicate a maximum offset of 7 meters (23 feet) in the central section of the break. 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