Advances in origin of high oxidation state of magmas associated with porphyry Cu-(Mo-Au) deposits  

作　　者：Rui WANG Jingbo ZHANG 

机构地区：[1]State Key Laboratory of Geological Processes and Mineral Resources,Frontiers Science Center for Deep-time Digital Earth,Institute of Earth Sciences,China University of Geosciences,Beijing 100083,China [2]School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China

出　　处：《Science China Earth Sciences》2025年第3期953-956,共4页中国科学(地球科学英文版)

基　　金：supported by the National Natural Science Foundation of China (Grant No. 42225204);the Fundamental Research Funds for the Central Universities (Grant No. 2652023001);the Program of Introducing Talents of Discipline to Universities (Grant No. B18048)。

摘　　要：1. Introduction Porphyry Cu-(Mo-Au) deposits, hereafter termed as porphyry Cu deposits, are typical magmatic-hydrothermal systems spatially and genetically associated with shallow,intermediate to felsic porphyritic intrusions. These deposits exhibit well-developed alteration zoning and are characterized by veinlet-disseminated mineralization.

关 键 词：PORPHYRY MAGMA DEPOSITS 

分 类 号：P618.41[天文地球—矿床学] P618.51[天文地球—地质学] P618.65