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  1. University of Yangon
  2. Department of Geology

Tin-tungsten Mineralization of Zingyaik-Kadaik Area, Paung Township, Mon State

http://hdl.handle.net/20.500.12678/0000002178
http://hdl.handle.net/20.500.12678/0000002178
55d42766-71b3-433b-a5b3-5e6c1eb22c9b
48f92d8e-0c3a-4acd-8eda-58aeb4463a57
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Tin-tungsten Tin-tungsten mineralization of Zingyaik-Kadaik Area, Paung Township, Mon State.pdf (4738 Kb)
Publication type
Journal article
Upload type
Publication
Title
Title Tin-tungsten Mineralization of Zingyaik-Kadaik Area, Paung Township, Mon State
Language en
Publication date 2008
Authors
Than Htoo Aung
Description
The research area is located near the Zingyaik and Kadeik villages, Paung Township, Mon State. It is situated within the western edges of the ShanThai Block composed mainly of slate, phyllitic slate, and quartzite units of Mergui Group which are intruded by the granitic rocks. The Tintungsten bearing veins occur in the granitoid and adjacent metasedimentary rocks along the Zingyaik range. These veins are trending NNW-SSE direction parallel to the regional structural trend. An alluvial Tin occurrence has been found near the Kadeik village. The Tin-tungsten mineralization occurs in the tourmaline-quartz veins, pegmatite and greisens. The alteration products of mineralization are silicification, tourmalinization, and g,reisenization. The Sn-W minerals associated with the pyrite, arsenopyrite, and chalcopyrite. Due to the XRF data, 0.125% to2.38 % of Sn and 2.125 % to 9.68 % of W were contained samples
from Zingyaik mine. The Tin-tungsten mineralization occurred as fracture filling ore deposits developed mainly along the NNW-SSE trending fault zones. According to the field evidences and laboratory analysis, tin-tungsten ore is formed at pneumatolitic to hypothermal stages in the magmatic hydrothermal system.
Keywords
Zingyaik-Kadaik area
Identifier https://uyr.uy.edu.mm/handle/123456789/572
Journal articles
2
Universities Research Journal (URJ)
Conference papaers
Books/reports/chapters
Thesis/dissertations
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