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Cochabamba Fault Zone : ウィキペディア英語版 | Cochabamba Fault Zone The Cochabamba Fault Zone or Cochabamba Shear Zone is an east-southeast trending zone of sinistral strike-slip faults near the city of Cochabamba in the Bolivian Andes. The movements along Cochabamba Fault Zone are related to the bend in the Andes from running in a north-west direction to a north-south direction at this latitude. The compression of the crust at the Arica Elbow causes part of the thrust belt in the Bolivian Andes to acquire a lateral movement to escape from the compression taking place along the elbow axis.〔Dewey and Lamb 1992. (Active tectonics of the Andes ). Tectonophysics.〕 ==See also==
*Atacama Fault *Geology of Bolivia
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Cochabamba Fault Zone」の詳細全文を読む
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