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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Bibliographic Details
Main Authors: Dhiti Tulyatid, Wanida Rangubpit
Other Authors: Mahidol University
Format: Article
Published: 2018
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Online Access:https://repository.li.mahidol.ac.th/handle/123456789/43144
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Institution: Mahidol University

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