Re-Os isotope dating of molybdenite from Shangalon Cu-Au deposit in the Wunto-Popa magmatic arc,Myanmar and its geological significance
The Shangalon copper-gold deposit is located in the northern segment of the Wunto-Popa magmatic arc in Myanmar.The research on this deposit is limited,and there is a lack of high-precision isotopic geochronological data regarding its ore-forming geological background and deposit genesis.In this study,five molybdenite samples from typical ores were selected to determine the mineralization age using the Re-Os isochron dating method.The obtained model ages range from 38.3±0.6 to 38.5±0.5 million years ago(Ma),with a weighted average age of 38.4±0.2 Ma.The corresponding isochron age is 38.0±1.6 Ma(MSWD=0.17).Both ages are in good agreement within the error range,indicating that the mineralization timing of the Shangalon copper-gold deposit is in the Eocene epoch.This age data corresponds well with the zircon U-Pb ages of 38 to 40 million years for the mineralized syenogranite and granodiorite in the mining area,suggesting a close relationship between the Shangalon Cu-Au-Mo mineralization and Eocene syenogranite-granodiorite intrusions,which are products of Eocene magmatic activity.The Re contents of molybdenite samples from the Shangalon copper-gold deposit range from 82.4 to 111.2 µg·g-1,with an average value of 98.88 µg·g-1,indicating a mixed source from the crust and mantle for the mineralizing fluids.Based on a comprehensive analysis of the regional metallogenic dynamics,it is suggested that the Eocene copper-gold mineralization in the Shangalon region possibly formed as a result of the fragmentation and faulting of the Neo-Tethys oceanic plate,triggered by the collision between the Indian and Eurasian continents,leading to upwelling of the asthenosphere and partial melting of the lower crust.
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