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Pinglu District (simplified Chinese: 平鲁区; traditional Chinese: 平魯區; pinyin: Pínglǔ Qū) is a district of the city of Shuozhou, Shanxi province, China, bordering Inner Mongolia to the northwest.
The estimated magnitude for this earthquake is about 6.8 M s . The earthquake is thought to have ruptured the Sanmenxia-lingbao Fault, with a normal fault mechanism. An analysis of the evolution of stresses following the 1303 earthquake at Hongdong, suggest that most of the earthquakes in the rift system can be explained by progressive coulomb stress transfer, although the main earthquake to ...
Map of the Shanxi Rift System along the eastern margin of the Ordos Block. The Shanxi Rift System or Fen–Wei Rift System [1] is a zone of active extensional tectonics that forms the eastern margin of the Ordos Block in northern China. The zone extends for at least 900 km (560 mi) and runs south-southwest to north-northeast.
Pinglu County (simplified Chinese: 平陆县; traditional Chinese: 平陸縣; pinyin: Pínglù Xiàn) is a county in southern Shanxi province of China. It is under the administration of the prefecture-level city of Yuncheng and has a population of approximately 200,000 people. Pinglu is historically an agricultural county, producing apples ...
African Rift Valley. From left to right: Lake Upemba, Lake Mweru, Lake Tanganyika (largest), and Lake Rukwa. A rift valley near Quilotoa, Ecuador. The Ottawa-Bonnechere Graben Þingvallavatn. A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift.
Pinglu may refer to: Pinglu County, in Shanxi, China; Pinglu District, in Shuozhou, Shanxi, China; Pinglu Canal (平陆运河), under-construction canal in Guangxi
The Midcontinent Rift System (MRS) or Keweenawan Rift is a 2,000 km (1,200 mi) long geological rift in the center of the North American continent and south-central part of the North American plate. It formed when the continent's core, the North American craton , began to split apart during the Mesoproterozoic era of the Precambrian , about 1.1 ...
Block view of a rift formed of three segments, showing the location of the accommodation zones between them at changes in fault location or polarity (dip direction) Gulf of Suez Rift showing main extensional faults. In geology, a rift is a linear zone where the lithosphere is being pulled apart [1] [2] and is an example of extensional tectonics ...