Evolution of a major extensional boundary fault system during multi-phase rifting in the Songkhla Basin, Gulf of Thailand
© 2018 Elsevier Ltd The Cenozoic N-S trending Songkhla rift basin, located in the southwest Gulf of Thailand, is a half-graben structure. The boundary fault zone on the western side of the basin is formed from a series of N-S to NNE-SSW, east-dipping normal faults. The Songkhla basin is an example o...
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| 格式: | 雜誌 |
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2018
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| 在線閱讀: | https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85053145804&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/62693 |
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| 機構: | Chiang Mai University |
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