Since the Wenchuan earthquake on May 12, 2008, abundant studies of the formation mechanism of earthquakes along the LMSF were performed. Mid Strike-slip faults have walls that move sideways, not up or down. The quake was caused by the collision of the Indian-Australian and Eurasian plates along the 155-mile- (249-km-) long Longmenshan Fault, a thrust fault in which the stresses produced by the northward-moving Indian-Australian plate shifted a portion of the Plateau of Tibet eastward. Compositional, mechanical and transport properties of carbonate fault rocks and the seismic cycle in limestone terrains : A case study of surface exposures on the Longmenshan Fault, Sichuan, China The southern part of the Longmenshan fault zone is complex and still only moderately understood. Knowledge of the nature and history of the LFZ is important for understanding the growth of continental plateaus and mechanisms for major earthquakes along their margins, as exemplified by the magnitude 7.9 M Wenchuan earthquake of 12 May 2008. This fault is most likely a normal fault reverse fault strike-slip fault This belt is mainly composed of 4 faults from the west to the east, which are Maoxian-Wenchuan fault, Beichuan-Yingxiu fault, An integrated analysis of high‐resolution remote sensing image interpretation, mainshock and aftershock distribution, and focal mechanism solutions indicated that this earthquake was an independent rupturing event in the southwestern segment of the Longmenshan fault zone, belonging to the thrust‐type earthquake. In May 2008, a magnitude-7.9 earthquake struck near Wenchuan, China, killing more than 80,000 people in the country’s biggest quake since 1950. And transverse faults can be divided into regional transverse faults and localized transverse faults with NW strike, nearly EW strike and nearly SN strike. [cite journallast = Dong Jia et al. The seismicity of Longmenshan fault zone and its vicinities before the 12 May 2008 Wenchuan MS8.0 earthquake is studied. If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the left block moves toward you and the right block moves away A right-lateral strike-slip fault If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the right block moves toward you and the left block moves away. Together these data suggest that thrust faults in the Longmenshan join to form a décollement at mid-crustal depths beneath the eastern Tibetan Plateau (Yu et al., 2010). Normal Fault Animation. reported for the first time the co-seismic graphitization occurred within the CM-rich gouge of WFSD-1. If you would like to participate, you can choose to edit this article, or visit the project page for more information. Abstract. Research shows that there are 9 transverse faults that lie parallel to each other approximately at ~50km intervals in the Longmenshan fault zone. The Longmenshan Fault is in China. title = Longmen Shan fold-thrust belt and its relation to the western Sichuan Basin in central China: New insights from hydrocarbon exploration thrust fault - a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block. This belt is mainly composed of 4 faults from the west to the east, which are Maoxian-Wenchuan fault, Beichuan-Yingxiu fault, Anxian-Guanxian fault and Guangyuan-Dayi fault, respectively (Hubbard et al., 2008; Xu et al., 2008). The Longmenshan fault zone is located at the Eastern Tibet, north from the Qingchuan, go through the Nanba, Beichuan, Yingxiu, Baoxing to LuDing, total length is about 560 km, and width is 30-50 km. 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