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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
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4c5515ec-b56c-45de-bb40-f729d7858c9e
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The The Study of folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division.pdf (4769 Kb)
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Journal article
Upload type
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
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0
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