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  1. University of Yangon
  2. Department of Geology

A Study on the Geology and Petrography of Lead Mineralization in Mogyo Taung and Peikchin Ganaing Taung areas, Ywangan Township, Taunggyi District, Shan State (South)

https://meral.edu.mm/records/9376
https://meral.edu.mm/records/9376
983b96dc-8e0e-4a71-9120-b7b1919c489e
91b33ee3-d4c9-4f03-819a-3e03c88c5adf
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Title
Title A Study on the Geology and Petrography of Lead Mineralization in Mogyo Taung and Peikchin Ganaing Taung areas, Ywangan Township, Taunggyi District, Shan State (South)
Language en
Publication date 2022-12-31
Authors
Aye Khaing
Description
The study areas, Mogyo Taung and Peikchin Ganaing Taung Areas, lie within the Pindaya Anticline in Ywanagn Township, Taunggyi District, Shan State (south). It is located about 25 kilometers northeast of Ywangan. It covers about 64 square kilometers in Universal Traverse Mercator map sheet No. 2196 /11-12. It is also located between latitude 21°00´ - 21°30´ and longitude 96°15´ - 96°45´. The physiography of the study area is mountainous, and the Mogyo Taung range is trending NNW- SSE. The highest part of the study area is the peak of the Ngwetaunggyi Taung range (1714 metres). Generally, the Pindaya Range is a south-plunging anticlinal fold, but the northern half of the range is very complex, having overturned and recumbent folds and systems of faults in diagonal directions. Pindaya-Kaungpo fault, nearly parallel to the major fold axis of the Pindaya Anticline. The Karani Fault and the Ingyi-Ingaung Fault are trending nearly N-S. Major rock units exposed in the study area and its surrounding environs overlying the Precambrian basement are the Molohein Group (Cambrian), Pindaya Group (Ordovician), Mibayataung Group (Silurian), and Plateau Limestone Group (Early Permian - Middle Triassic). The rocks of the Mibayataung Group are unconformable and overlained by the Plateau Limestone Group. The study area comprises the Pindaya Group (Lokepyin, Wunbye, and Nan-on Formations) and the Mibayataung Group (Linwe, Wabya Formations). The present research work involves the carbonate rocks of the Wunbye Formation (Middle Ordovicain age), and has five microfacies, namely, oolitic-dolomitized grainstone, dolomitic limestone, dolostone, oolitic- peloidal grainstone and peloidal- bioclastic wackestone.
Keywords
Mogyo Taung, Peikchin Ganaing Taung, Pindaya Group (Ordovician)
Journal articles
2022
University of Yangon Research Journal
469-482
11, No. 1
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