Pre-seismic deformation detected from regional GNSS observation network: A case study of the 2013 Lushan, eastern Tibetan Plateau (China), select article Electrical structure of the Kunlun–Qinling fault system, northeastern Tibetan Plateau, inferred from 3-D inversion of magnetotelluric data, Electrical structure of the Kunlun–Qinling fault system, northeastern Tibetan Plateau, inferred from 3-D inversion of magnetotelluric data, select article Inversion of the rupture process and high-frequency radiation of the 2017 Jiuzhaigou earthquake, northeastern Tibetan Plateau, Inversion of the rupture process and high-frequency radiation of the 2017 Jiuzhaigou earthquake, northeastern Tibetan Plateau, select article Transformation of coseismic faults in the northern Longmenshan tectonic belt, eastern Tibetan Plateau: Implications for potential earthquakes and seismic risks, Transformation of coseismic faults in the northern Longmenshan tectonic belt, eastern Tibetan Plateau: Implications for potential earthquakes and seismic risks, select article Paleoseismic events on the Shuangshi-Dachuan fault of the seismic gap, Longmen Shan thrust belt, eastern margin of the Tibetan Plateau, Paleoseismic events on the Shuangshi-Dachuan fault of the seismic gap, Longmen Shan thrust belt, eastern margin of the Tibetan Plateau, select article 3D geometry of range front blind ramp and its effects on structural segmentation of the southern Longmen Shan front, eastern Tibet, 3D geometry of range front blind ramp and its effects on structural segmentation of the southern Longmen Shan front, eastern Tibet, select article Differential strain transfer, Longmen Shan thrust belt, eastern Tibetan Plateau margin: Implications for seismic hazards, Differential strain transfer, Longmen Shan thrust belt, eastern Tibetan Plateau margin: Implications for seismic hazards, select article Electrical resistivity structure of the Xiaojiang strike-slip fault system (SW China) and its tectonic implications, Electrical resistivity structure of the Xiaojiang strike-slip fault system (SW China) and its tectonic implications, select article Late Quaternary slip rates and Holocene paleoearthquakes of the eastern Yumu Shan fault, northeast Tibet: Implications for kinematic mechanism and seismic hazard, Late Quaternary slip rates and Holocene paleoearthquakes of the eastern Yumu Shan fault, northeast Tibet: Implications for kinematic mechanism and seismic hazard, select article Seismic effects of a small sedimentary basin in the eastern Tibetan plateau based on numerical simulation and ground motion records from aftershocks of the 2008 Mw7.9 Wenchuan, China earthquake, Seismic effects of a small sedimentary basin in the eastern Tibetan plateau based on numerical simulation and ground motion records from aftershocks of the 2008 Mw7.9 Wenchuan, China earthquake.
The Longmenshan Fault on the latter border was the site of the 2008 Wenchuan earthquake.
Areas of maximal intensity were mainly distributed around the estuary of the Yellow River.
Therefore, Longmenshan formation and its internal fractures constitute a special type that has low earthquake frequences but the potential to cause super strong earthquakes. About 1.2 billion people speak some form of Chinese as their first language.
(dip-slip) 3. Regional topographic gradients typically exceed 10% along this mountain front and rival any other margin of the plateau." 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. The upper block moves downward relative to the lower block.
Since Holocene (10,000), Yingxiu-Beichuan fracture has had evident activities. 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. By signing up for this email, you are agreeing to news, offers, and information from Encyclopaedia Britannica.
[5]. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. The magnitude of this earthquake is Ms 7.4. It was located near Litang, China. The upper block moves upward relative to the lower block.
The China Earthquake Administration (CEA), is mandated by the Law of the People's Republic of China on Protecting Against and Mitigating Earthquake Disasters of PRC to enforce the earthquake administration in the nation under the administration of State Council of the People's Republic of China. With more than 400 aftershocks, it caused over 40 deaths, the collapse of 10,000 homes and damage to other infrastructure in the area. We used a total of 8589 P wave arrival times from 1014 local earthquakes recorded by both the Zipingpu reservoir network and temporary stations deployed in the area. It is famous for its rice cultivation and is often considered the breadbasket of China. Three-dimensional P wave velocity models under the Zipingpu reservoir in Longmenshan fault zone are obtained with a resolution of 2 km in the horizontal direction and 1 km in depth. Channel flow and fault segmentation with implications for the generation of earthquakes in the Longmenshan fault zone, eastern Tibetan Plateau Peng Fang, Guiting Hou 15 June 2019 [1] Motion on this fault is responsible for the uplift of the mountains relative to the lowlands of the Sichuan Basin to the east. It stretches approximately 1,000 kilometres (620 mi) north to south and 2,500 kilometres (1,600 mi) east to west. Announcing our NEW encyclopedia for Kids! The Sichuan Basin, formerly transliterated as the Szechwan Basin, sometimes called the Red Basin, is a lowland region in southwestern China.
In this study, continuous seismic … Elevations rise from circa 600 m in the southern Sichuan Basin to peaks exceeding 6500 m over a horizontal distance of less than 50 km. Both blocks slide horizontally across one another. The epicenter was located in the Bohai Sea, off the coast of Shandong Province, China. On June 9 2008, more than 250,000 people have been evacuated from Mianyang in anticipation of the Tangjiashan Lake dam bursting.
Coordinates: 30°N105°E / 30°N 105°E / 30; 105, CS1 maint: Multiple names: authors list (, "Longmen Shan fold-thrust be ilt and its relation to the western Sichuan Basin in central China: New insights from hydrocarbon exploration", "汶川8.0級地震成因分析 (Cause Analysis of the M8.0 Wenchuan earthquake)", "Late Cenozoic evolution of the eastern margin of the Tibetan Plateau", Simplified geologic map of the Longmen Shan region, China Virtual Museum of Earthquakes, map charting the. The epicenter was located in Lushan County, Ya'an, Sichuan, about 116 km (72 mi) from Chengdu along the Longmenshan Fault in the same province heavily impacted by the 2008 Sichuan earthquake. [2]. The city proper is subdivided into four urban districts and has jurisdiction over 21 towns, and 19 rural townships. [1] Motion on this fault is responsible for the uplift of the mountains relative to the lowlands of the Sichuan Basin to the east. On May 24, 2008 the water level rose by 2 metres in a single day, reaching a depth of 23 metres (75 ft), just 29 metres (95 ft) below the barrier level. Its long-term geological slip rate is slower than 1 mm per year. By continuing you agree to the use of cookies. Its tens of thousands of glaciers and other geographical and ecological features serve as a "water tower" storing water and maintaining flow. Ten people were reported dead. The epicenter was located in the area around Lazha (拉鲊), Dalongtan (大龙潭) Township, Renhe District, Panzhihua and Yuzha (鱼鲊) Township, Huili County.
The earthquake ruptured the fault for over 240 km (150 mi), with surface displacements of several meters.
Beichuan Earthquake Museum (北川国家地震遗址博物馆) is a memorial museum of the 2008 Wenchuan earthquake located in Beichuan County, Sichuan, China.
Representing the eastern boundary of the Qinghai-Tibet Plateau, it is a border formation between the Bayan Kola block in the Plateau and the South China block in the Eurasian Plate. The Longmenshan fault zone consists of the Back-range, the Central and the Front-range faults. Its new county seat is located at Yongchang after the 2008 Sichuan earthquake. Due to its relative flatness and fertile soils, it is able to support a population of more than 100 million.
Both the 2008 Wenchuan earthquake and the 2013 Ya'an earthquake occurred along this fault. The 1994 Taiwan Strait earthquake occurred on 16 September 1994, at 14:20 local time in the southern Taiwan Strait. It is bordered by the prefecture-level divisions of Deyang to the northeast and the Ngawa Tibetan and Qiang Autonomous Prefecture to the north. It has an area of 1,208 km2 (466 sq mi) and had a population of 600,000 in 2003.
The 2008 Panzhihua earthquake struck southern Sichuan province, China on August 30 at 16:30:50.5 China Standard Time with a surface wave magnitude of 6.1.
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