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The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division
http://hdl.handle.net/20.500.12678/0000002559
http://hdl.handle.net/20.500.12678/0000002559826d78e6-1112-4447-a6d1-44c3bd18c9cd
4c5515ec-b56c-45de-bb40-f729d7858c9e
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Journal article | ||||||
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Publication | ||||||
Title | ||||||
Title | The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division | |||||
Language | en | |||||
Publication date | 2008 | |||||
Authors | ||||||
Saw Ngwe Khaing | ||||||
Description | ||||||
The Pinle-in area is mainly composed of metasedimentary rocks with some igneous intrusions. It is situated between Sagaing Fault and Shan-Scarp Fault in central Myanmar. The present study has carried out the systematic measurements of the plunge directions, plunge angles, thickness and distance of the limbs of minor folds in the calc-silicate rocks of Pinle-in area, Madaya and Singu Township, Mandalay Division. Similar plunge directions of folds are grouped as the zones. These zones are matched to speculate the possible explanation for where the hidden major fold is situated. The type of folds may be more or less anticline preferably overturned natures in the area. The axis of overturned anticline, likely to be double plunging, may be located along the Thabyaw Range with the direction of NNW-SSE and the Yetkanzin Range may also be assumed as the southern continuation of the Thabyaw Range. | ||||||
Keywords | ||||||
Minor folds | ||||||
Identifier | https://uyr.uy.edu.mm/handle/123456789/571 | |||||
Journal articles | ||||||
2 | ||||||
Universities Research Journal (URJ) | ||||||
Conference papaers | ||||||
Books/reports/chapters | ||||||
Thesis/dissertations |