Jump to content

Cochabamba Fault Zone

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Nemo bis (talk | contribs) at 09:30, 28 July 2019 (Alter: pages. Add: issue. Removed URL that duplicated unique identifier. Formatted dashes. | You can use this tool yourself. Report bugs here.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

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.[1]

See also

References

  1. ^ Dewey, J.F; Lamb, S.H (1992), "Active tectonics of the Andes", Tectonophysics, 205 (1–3): 79–95, doi:10.1016/0040-1951(92)90419-7