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Magmatic‐Fluid‐Metallogenic System of the Anqing Skarn Cu‐Fe Deposit, Anhui Province, China
Author(s) -
YANG Guangshu,
WEN Hanjie,
YAN Yongfeng,
FENG Pengyu,
ZHANG Junwei
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12385_52
Subject(s) - skarn , china , geochemistry , geology , mining engineering , geography , fluid inclusions , archaeology , paleontology , quartz
The Anqing skarn-type Cu-Fe deposit is an important part of Tongling-Anqing iron-copper mineralization concentration field. Over the last few decades, several metallogenic models have been proposed (Zhou et al., 2007; Yang, et al., 2008). However, the source of oreforming materials and the fluid system of mineralization are controversial (Zhang et al., 2012). This paper represents the characteristics of ore-forming fluid and C-O isotope compositions in the Anqing Cu-Fe deposit, and tries to use these data to discuss and understand the magmaticfluidmetallogenic system of this deposit.