It is surrounded by mountains on all sides and is drained by the Yangtze River and its tributaries. The upper block moves upward relative to the lower block. Strong aftershocks, some exceeding 6 Ms, continued to hit the area up to several months after the main shock, causing further casualties and damage. The epicenter was located in the Bohai Sea, off the coast of Shandong Province, China. 1,815 aftershocks have been recorded as of 00:00 (UTC+8h) April 22. The basin is anchored by Chengdu, capital of Sichuan province, in the west, and the independent municipality of Chongqing in the east. Pengzhou, formerly Peng County or Pengxian, is a county-level city under the jurisdiction of Chengdu, the capital of Sichuan province, People's Republic of China, some 19 km (12 mi) northwest of Chengdu. The 2008 Sichuan earthquake, also known as the Great Sichuan earthquake or Wenchuan earthquake, occurred at 14:28:01 China Standard Time on May 12, 2008. It is located at the southern end of the Ngawa Tibetan and Qiang Autonomous Prefecture, and lies on the road to Jiuzhaigou Valley, Wolong and the Siguniang Mountains. The 1948 Litang earthquake (1948年理塘地震) occurred on May 28, 1948 at 07:11 UTC. [2]. The impact of global warming on the Tibetan Plateau is of intense scientific interest. In the 21st century its industrial base is expanding with growth in the high-tech, aerospace, and petroleum industries. Dujiangyan is a county-level city, a subdivision of Chengdu, the capital of Sichuan Province, People's Republic of China. The 1969 Bohai earthquake occurred on July 18, 1969, at 13:24 local time. Due to its relative flatness and fertile soils, it is able to support a population of more than 100 million. It is also cited as the Renhe-Huili earthquake, especially in SCEA reports and early CEA reports. Compressional forces brought on by this shift sheared the ground in two locations along the fault, thrusting the ground upward by…. The 2017 Jiuzhaigou earthquake occurred on 8 August 2017, in Zhangzha Town, Jiuzhaigou County, Ngawa Prefecture, Sichuan Province, China. A magnetotelluric (MT) study was undertaken subsequent to the earthquake to investigate the crustal structure of the Longmenshan, and inversion of the data reveals a low-resistivity (high-conductivity) layer at a depth of ∼20 km beneath the eastern Tibetan Plateau that terminates ∼25 km west of the Wenchuan-Maoxian fault. In addition to being a dominant geographical feature of the region, the Sichuan Basin also constitutes a cultural sphere that is distinguished by its own unique customs, cuisine, and dialects. It is located 47 kilometres (29 mi) south of the county urban centre, and just 14 kilometres (8.7 mi) west of the city of Dujiangyan. The magnitude of the earthquake was placed at Ms 7.0 by China Earthquake Data Center, Ms 7.0 by Russian Academy of Sciences, Mw 7.0 by Geoscience Australia, Mw 6.6 by the United States Geological Survey (USGS), Mw 6.6 by the European Alert System (EMSC) and Mj 6.9 by the Japan Meteorological Agency (JMA). Strike-slip fault.
After the May 12, 2008, earthquake in the Chinese province of Sichuan, there was a series of allegations of corruption against officials involved in the construction of schools in regions affected by the quake. With an average elevation exceeding 4,500 metres (14,800 ft), the Tibetan Plateau is sometimes called "the Roof of the World" because it stands over 3 miles (4.8 km) above sea level and is surrounded by imposing mountain ranges that harbor the world's two highest summits, Mount Everest and K2, and is the world's highest and largest plateau, with an area of 2,500,000 square kilometres (970,000 sq mi). It is bordered by the prefecture-level divisions of Deyang to the northeast and the Ngawa Tibetan and Qiang Autonomous Prefecture to the north.
Beichuan Qiang Autonomous County is a county under the jurisdiction of Mianyang City in northern Sichuan province, China. The mechanism of this earthquake was of dextral strike-slip faulting. Receive an update when the latest issues in this journal are published, https://doi.org/10.1016/j.jseaes.2020.104474, https://doi.org/10.1016/j.jseaes.2019.103941, Guangbao Du, Qingju Wu, Xuemei Zhang, Jing He, ... Fabio Romanelli, https://doi.org/10.1016/j.jseaes.2020.104230, Muyu Tian, Zhouchuan Huang, Liangshu Wang, Mingjie Xu, ... Yajing Bi, https://doi.org/10.1016/j.jseaes.2019.104027, https://doi.org/10.1016/j.jseaes.2019.02.003, Xin Wang, Jingfa Zhang, Wenliang Jiang, Dehua Wang, https://doi.org/10.1016/j.jseaes.2019.103887, https://doi.org/10.1016/j.jseaes.2020.104429, Chengjun Feng, Yihai Yang, Xiaodong Ma, Bangshen Qi, ... 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Wen Nie, select article Preface to the special issue on Structure and dynamics of the Longmenshan fault zone, Preface to the special issue on Structure and dynamics of the Longmenshan fault zone, select article Pn wave velocity and anisotropy underneath the central segment of the North-South Seismic Belt in China, Pn wave velocity and anisotropy underneath the central segment of the North-South Seismic Belt in China, select article Tectonic evolution of the eastern margin of the Tibetan plateau: Insight from crustal structures using P wave receiver functions, Tectonic evolution of the eastern margin of the Tibetan plateau: Insight from crustal structures using P wave receiver functions, select article Frequency-dependent Pms splitting measurements across the Longmenshan thrust belt in the eastern Tibetan Plateau, Frequency-dependent Pms splitting measurements across the Longmenshan thrust belt in the eastern Tibetan Plateau, select article Gravity field and deep seismogenic environment in the Longmen Shan and adjacent regions, Eastern Tibetan Plateau, Gravity field and deep seismogenic environment in the Longmen Shan and adjacent regions, Eastern Tibetan Plateau, select article A study of site response and regional attenuation in the Longmen Shan region, eastern Tibetan Plateau, SW China, from seismic recordings using the generalized inversion method, A study of site response and regional attenuation in the Longmen Shan region, eastern Tibetan Plateau, SW China, from seismic recordings using the generalized inversion method, select article Local stress perturbations associated with the 2008 Wenchuan M 8.0 earthquake near the Longmenshan fault zone in the eastern margin of the Tibetan Plateau, Local stress perturbations associated with the 2008 Wenchuan, select article Electrical Constraints on the channel flow underneath the northeastern Tibetan plateau: Results of the Longriba-Minjiang magnetotelluric sounding profile, Electrical Constraints on the channel flow underneath the northeastern Tibetan plateau: Results of the Longriba-Minjiang magnetotelluric sounding profile, select article Contrasting crustal deformation mechanisms in the Longmenshan and West Qinling orogenic belts, NE Tibet, revealed by magnetotelluric data, Contrasting crustal deformation mechanisms in the Longmenshan and West Qinling orogenic belts, NE Tibet, revealed by magnetotelluric data, select article Late Cenozoic structural deformation and evolution of the central-southern Longmen Shan fold-and-thrust belt, China: Insights from numerical simulations, Late Cenozoic structural deformation and evolution of the central-southern Longmen Shan fold-and-thrust belt, China: Insights from numerical simulations, select article 3D geometric modeling for the Yanjinggou anticline in the Longmen Shan fold-and-thrust belt, China: Oblique thrusting kinematic implications, 3D geometric modeling for the Yanjinggou anticline in the Longmen Shan fold-and-thrust belt, China: Oblique thrusting kinematic implications, select article Evidence for three Cenozoic phases of upper crustal shortening of the Xiongpo structure in the Longmen Shan fold-and-thrust belt, China: Implications for the eastward growth of the eastern Tibetan Plateau, Evidence for three Cenozoic phases of upper crustal shortening of the Xiongpo structure in the Longmen Shan fold-and-thrust belt, China: Implications for the eastward growth of the eastern Tibetan Plateau, select article Formation of the Late Triassic western Sichuan foreland basin of the Qinling Orogenic Belt, SW China: Sedimentary and geochronological constraints from the Xujiahe Formation, Formation of the Late Triassic western Sichuan foreland basin of the Qinling Orogenic Belt, SW China: Sedimentary and geochronological constraints from the Xujiahe Formation, select article Evidence for normal and deep-buried features of the Longquan Shan fault zone at the eastern margin of the Tibetan plateau, Evidence for normal and deep-buried features of the Longquan Shan fault zone at the eastern margin of the Tibetan plateau, select article The spatiotemporal strain partitioning across the Longmen Shan fault zone during seismic cycles: Implications for deformation mechanisms and seismicity in eastern Tibet, The spatiotemporal strain partitioning across the Longmen Shan fault zone during seismic cycles: Implications for deformation mechanisms and seismicity in eastern Tibet, select article Channel flow and fault segmentation with implications for the generation of earthquakes in the Longmenshan fault zone, eastern Tibetan Plateau, Channel flow and fault segmentation with implications for the generation of earthquakes in the Longmenshan fault zone, eastern Tibetan Plateau, select article Initial rupture processes of the 2008 Mw7.9 Wenchuan, China earthquake: From near-source seismic records, Initial rupture processes of the 2008 Mw7.9 Wenchuan, China earthquake: From near-source seismic records, select article The seismogenic structure of the southern segment of the Longmen Shan thrust belt, eastern Tibetan Plateau, SW China: A comprehensive analysis of surface geology and deep structure, The seismogenic structure of the southern segment of the Longmen Shan thrust belt, eastern Tibetan Plateau, SW China: A comprehensive analysis of surface geology and deep structure, select article Viscoelastic behavior of the crust around the Longmenshan Thrust Belt inferred from post-seismic deformation of the 2013 Lushan earthquake, China, Viscoelastic behavior of the crust around the Longmenshan Thrust Belt inferred from post-seismic deformation of the 2013 Lushan earthquake, China, select article Pre-seismic deformation detected from regional GNSS observation network: A case study of the 2013 Lushan, eastern Tibetan Plateau (China), Ms 7.0 earthquake.
Since Holocene (10,000), Yingxiu-Beichuan fracture has had evident activities. Jiangyou is noted as the hometown of Li Bai, a leading Tang Dynasty poet. Wenchuan County is a county in Ngawa Tibetan and Qiang Autonomous Prefecture, Sichuan, People's Republic of China.
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