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Fluid Inclusion Study of Gold Mineralization at the Taungzaw Area, Kanbalu Township, Sagaing Region, Myanmar
https://meral.edu.mm/records/9375
https://meral.edu.mm/records/93753aa595bf-99af-45f1-b82e-51db116ba5be
12ff708a-fd59-4f9f-9090-a2bde27ebcee
Name / File | License | Actions |
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Fluid Inclusion Study of Gold Mineralization at the Taungzaw Area, Kanbalu Township, Sagaing Region, Myanmar | |||||
Language | en | |||||
Publication date | 2024-03-20 | |||||
Authors | ||||||
Aung Myo Kyaw | ||||||
Day Wa Aung | ||||||
Description | ||||||
The Taungzaw area is located in Kanbalu Township, Sagaing Region, the Northern Myanmar. It lies in the eastern trough of the Central Myanmar Basin. Gold mineralization at the Taungzaw prospect occurs as a stockworks/dissemination style with localized breccia zones in silicified sandstone of the Eocene Male Formation. The mineralization appears to be closely associated with NNE-SSW trending extensional fault, which is probably related directly to the dextral movement of the Sagaing Fault system. Intense silicification associated with sericitization, argillic alteration, and decalcification is recognized in the ore zone. The gold grade is around 2.5 to 3g/t. The important ore minerals associated with gold mineralization are pyrite, chalcopyrite and arsenopyrite. Gold occurs as free particles or encapsulated with pyrite, chalcopyrite, arsenopyrite and tetrahedrite. Silver, copper, arsenic and antimony particularly appear to be good pathfinders and the best geochemical indicators of the gold mineralization. The fluid inclusion micro thermometric study indicates that the ore mineralization is characterized by the temperature of homogenization ranging from 162.2 and 256.3ºC and salinities ranging from 0.71 to 2.54wt.% NaCl equivalent. According to the fluid inclusion study, micro thermometry measurements and ore minerals assemblage and paleo-depth estimation, and hydrothermal alteration types of the Taungzaw prospect imply formation under an epithermal environment. | ||||||
Keywords | ||||||
Central Myanmar Basin, epithermal environment, Male Formation, Sagaing Fault, Taungzaw area Introduction | ||||||
Journal articles | ||||||
2022 | ||||||
University of Yangon Research Journal | ||||||
455-468 | ||||||
11, No. 1 |