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: | , |
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| Language: | English |
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Science Faculty of Chiang Mai University
2020
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| Online Access: | http://epg.science.cmu.ac.th/ejournal/dl.php?journal_id=7613 http://cmuir.cmu.ac.th/jspui/handle/6653943832/67360 |
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| Institution: | Chiang Mai University |
| Language: | English |
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