Structural geometry and timing of deformation in the Chainat duplex, Thailand
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...
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| Main Authors: | , , , |
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| 格式: | Conference or Workshop Item |
| 語言: | English |
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2014
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| 在線閱讀: | http://www.scopus.com/inward/record.url?eid=2-s2.0-38549139498&partnerID=40&md5=3663993c3f0e9eddb2743c54347eaab2 http://cmuir.cmu.ac.th/handle/6653943832/5161 |
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