中国地质(英文) · 2020年第2期348-349,共2页

Zircon O isotope composition of Sepon Au-Cu deposit, Laos

作者:Xin-yu Wang,Dian-hua Cao,Jian-hua Wang

摘要:1.Objective The Sepon Au-Cu deposit(Fig.1)is the largest polymetal deposit ever discovered in Laos,of which the resources of gold and copper is 102 t(Au:1.6 g/t)and 1.96×10^6 t(TCu:2%)(Zhu HP et al.,2013)respectively.Sepon Au-Cu deposit is one of the most important super large deposits of the Truong Son Fold Belt.The Truong Son Fold Belt,located at the northeastern margin of the Indo-China terrane,is considered to be tectonically linked to the subduction of the Paleotethys Ocean and subsequent collision.The granodiorite porphyry samples from the Sepon deposit belong to I-type calc-alkaline series and tectonic settings are continental arc environment(Cromie PW,2010).LA-ICP MS zircon U-Pb dating results show that granodiorite porphyry samples from the Sepon deposit have ages of 302.1±2.9 Ma.The in situ zirconεHf(t)values range from+4.32 to+9.64,and TDM2(Hf)has an average age of 914 Ma(Wang XY et al.,2018).In this study,the authors present new in situ zircon oxygen isotopic data to identify the source of the magma.

发文机构:Chinese Academy of Geological Sciences Ministry of Natural Resources Key Laboratory of Metallogeny and Mineral Assessment Department of Terrestrial Magnetism

关键词:DEPOSITZIRCONTECTONIC

分类号: P59[天文地球—地球化学]

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