Re-Os Geochronology of Molybdenite from Yinyan Porphyry Sn Deposit in South China

Abstract

The Yinyan Sn deposit, one of the three typical porphyry Sn deposits in China, is located in the western Guangdong province of the Cathaysia Block. Rhenium and osmium isotopes of molybdenites from the Yinyan deposit were first used to constrain the age of mineralization. Rhenium concentrations in molybdenite samples range from 0.13 to 1.3μgg-1, indicating a crustal source for the ore-forming materials. The Re-Os dating yield model ages ranging from 78.1 to 79.52Ma, with an average of 78.65±0.98Ma, and give an isochron age of 78.8±2.6Ma. Evidently, isochron age is consistent with model ages in the error within the allowable range, so we can constrain the precise age of Yinyan Sn deposit at the Late Cretaceous. Based on the geological history and spatial-temporal distribution of the Sn deposits, it is proposed that the formation of Sn deposits in the Cathaysia Block were related to lithospheric extension that are associated with a change in the polarity of the subduction of the Paleo-Pacific Plate from oblique subduction to parallel the eastern margin of the Eurasian Plate after 135Ma. The Yinyan porphyry Sn deposit is located in the western Guangdong province of the Cathaysia block. The Re-Os average model age of molybdenite associated with cassiterite from Yinyan Sn deposit is 78.65±0.98 Ma. Sn deposits in the Cathaysia block were related to lithospheric extension that are related to a change in the polarity of the subduction of the Paleo-Pacific Plate from oblique subduction to parallel the eastern margin of the Eurasian after 135 Ma.