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

• المؤلفون الرئيسيون: Morley C.K., Smith M., Carter A., Charusiri P., Chantraprasert S.
• مؤلفون آخرون: Cunningham W.D.Mann P.
• التنسيق: Conference or Workshop Item
• اللغة: English
• منشور في: 2014
• الوصول للمادة أونلاين: http://www.scopus.com/inward/record.url?eid=2-s2.0-38549171284&partnerID=40&md5=5b5fb9e64961cae5432ef228c8956d81; http://cmuir.cmu.ac.th/handle/6653943832/5124

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...