Structural geometry and timing of deformation in the Chainat duplex, Thailand

• المؤلفون الرئيسيون: Smith M., Chantraprasert S., Morley C.K., Cartwright I.
• 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-s2.0-38549139498&partnerID=40&md5=3663993c3f0e9eddb2743c54347eaab2; http://cmuir.cmu.ac.th/handle/6653943832/5161
• المؤسسة: Chiang Mai University

The Chainat duplex is about 100 km in a north-south direction, and was developed along the predominantly sinistral Mae Ping fault zone, which was active during the Cenozoic. The duplex is manifested as eroded, north-south- and NW-SE-striking outliers of Palaeozoic and Mesozoic rocks rising from the...