Evolution of deformation styles at a major restraining bend, constraints from cooling histories, Mae Ping fault zone, western Thailand

Evolution of deformation styles at a major restraining bend, constraints from cooling histories, Mae Ping fault zone, western Thailand

The c. 500-km-long Mae Ping fault zone trends NW-SE across Thailand into eastern Myanmar and has probably undergone in excess of 150 km sinistral motion during the Cenozoic. A large, c. 150-km-long, restraining bend in this fault zone lies on the western margin of the Chainat duplex. The duplex is a...

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Bibliographic Details
Main Authors: Chriss K. Morley, M. Smith, A. Carter, P. Charusiri, S. Chantraprasert
Format: Book Series
Published: 2018
Subjects:
Earth and Planetary Sciences
Engineering
Environmental Science
Online Access:https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=38549171284&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/61016
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Institution: Chiang Mai University

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http://cmuir.cmu.ac.th/jspui/handle/6653943832/61016

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