Structural geometry and timing of deformation in the Chainat duplex, Thailand
The Chainat duplex is about 100 km in a north-south direction, and was developed along the predominantly sinistral Mae Ping fault zone, which was active during the Cenozoic. The duplex is manifested as eroded, north-south- and NW-SE-striking outliers of Palaeozoic and Mesozoic rocks rising from the...
Saved in:
| Main Authors: | , , , |
|---|---|
| Format: | Book Series |
| Published: |
2018
|
| Subjects: | |
| Online Access: | https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=38549139498&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/61015 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Institution: | Chiang Mai University |