Subsurface structure of Kanchanaburi area interpreted from aeromagnetic data
© 2016, Chiang Mai University. All rights reserved. The Three Pagoda Fault Zone (TPFZ) is believed to have developed as a consequence of the Indian-Eurasian Collision, and is considered to originally have been a major left lateral shear zone activated during the Eocene - Oligocene. The fault zone pr...
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Format: | Article |
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2018
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Online Access: | https://repository.li.mahidol.ac.th/handle/123456789/43144 |
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Institution: | Mahidol University |