Syn-mineralization Uplifting and Exhumation of Porphyry Systems in China:Evidence from Fluid Inclusion Data  

作　　者：ZHOU Aorigele ZHENG Ming TANG Juxing HE Wen CHEN Hongjin 

机构地区：[1]MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China

出　　处：《Acta Geologica Sinica(English Edition)》2022年第1期240-247,共8页地质学报（英文版）

基　　金：financially supported by National Key R&D Program of China(2018YFC0604101,2018YFC0604106);National Natural Science Foundation of China(41902095)。

摘　　要：In order to understand how the metallogenic process of porphyry deposit specifically and directly respond to regional uplifting and exhumation,we compiled previous fluid inclusion data of 32 porphyry deposits in China by recalculating the fluid trapping depths and trapping depth reduction magnitude from early to late mineralization stage veins.The data reveal that the average trapping pressure ratio(Ave TP_(E)/TP_(L))between early-and late-stage veins of the these deposits are 1.2-18.4,mainly in the range of 1.35-5.83,with average trapping pressure reduction(1-Ave TP_(L)/TP_(E))from early-to late-stage veins are 17%-95%,and mainly in the range of 25%-83%.The fluid trapping pressure based mineralization depths most of the porphyry deposits in China had decreased from early to late vein stages by at least 450 m(900-5800 m predominant),or greater than 950 m when take the average depth reduction value,which is greater than the current gap between early-and late-stage veins of each deposit.We propose that the apparently greater mineralization depth reduction magnitude than the current elevation gaps between early and late veins are likely a consequence of synmineralization uplifting and exhumation process that often occurs in porphyry systems.

关 键 词：fluid inclusion syn-mineralization uplifting EXHUMATION porphyry deposit 

分 类 号：P612[天文地球—矿床学]