Subsurface structure of Kanchanaburi area interpreted from aeromagnetic data

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 probably reversed its movement to right lateral motio...

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Main Authors: Dhiti Tulyatid, Wanida Rangubpit
格式: บทความวารสาร
語言:English
出版: Science Faculty of Chiang Mai University 2019
在線閱讀:http://it.science.cmu.ac.th/ejournal/dl.php?journal_id=7613
http://cmuir.cmu.ac.th/jspui/handle/6653943832/63827
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機構: Chiang Mai University
語言: English