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Item
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Preliminary Study on Geology of Khwekha-Helok Area, Kalay and Falam Townships
http://hdl.handle.net/20.500.12678/0000000883
http://hdl.handle.net/20.500.12678/0000000883ec88e0c2-eb2f-4d4d-bfbf-35dd39b4a163
04a6bc2d-9547-4ba4-90af-635e305ca2d7
Name / File | License | Actions |
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Preliminary Study on Geology of Khwekha-Helok Area, Kalay and Falam Townships | |||||
Language | en | |||||
Publication date | 2010 | |||||
Authors | ||||||
Myo Min | ||||||
Lalrinchhana | ||||||
Zam Khan Mang | ||||||
Tin Warr Warr Min | ||||||
Man Deih Cing | ||||||
Description | ||||||
The study area is situated on the eastern flanks of the Chin Hills, about 20 km southwest of Kalaymyo. This area is generally trending SEE-NWW forming a north-south dipping isoclinals structure. In the study are, there are two main rock units are exposed; metasedimentary rocks and igneous rocks. Among the metasedimentary rocks, the schist unit is dominant that are quartz-rubellite schist, quartz-mica schist, hornblende schist, hornblende-epidote schist. The quartzite is exposed as a minor amount. These metasedimentary rocks are dated as Upper Triassic or older and probably derived from the ophiolite rock suite (basic and pellitic rocks). The igneous rocks units are mainly ultramafic rocks that comprise serpentinite, harzburgite and dunite. These ultramafic rocks intrude the metasedimnetary rocks and the age of intrusion may be late Cretaceous. | ||||||
Keywords | ||||||
Chin Hills | ||||||
Identifier | https://umoar.mu.edu.mm/handle/123456789/447 | |||||
Journal articles | ||||||
1 | ||||||
Banmaw University Research Journal | ||||||
2 | ||||||
Conference papaers | ||||||
Books/reports/chapters | ||||||
Thesis/dissertations |