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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| Main Authors: | , , , , |
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| Other Authors: | |
| Format: | Conference or Workshop Item |
| Language: | English |
| Published: |
2014
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| Online Access: | http://www.scopus.com/inward/record.url?eid=2-s2.0-38549171284&partnerID=40&md5=5b5fb9e64961cae5432ef228c8956d81 http://cmuir.cmu.ac.th/handle/6653943832/5124 |
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| Institution: | Chiang Mai University |
| Language: | English |