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Evolution of Ore‐forming Fluid of the Bafangshan‐Erlihe Pb‐Zn‐Cu Deposit in the Fengtai Ore Cluster, West Qinling, China: Evidence from Stable Isotopes and Fluid Inclusions
Author(s) -
HU Qiaoqing,
WANG Yitian,
LIU Xielu,
CHEN Shaocong,
WEI Ran,
ZHANG Juan,
WANG Ruiting,
DAI Junzhi,
WEN Shenwen,
WANG Shuangyan
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 - 10.1111/1755-6724.12369_11
Subject(s) - fluid inclusions , geochemistry , geology , ore genesis , isotope , metallurgy , materials science , hydrothermal circulation , paleontology , physics , quantum mechanics
cluster) in the Shaanxi Province, located in the middlewest of Qinling orogen, is an important part of the Qinling Pb-Zn-Au metallogenic belt. The Bafangshan-Erlihe PbZn-Cu deposit of the Fengtai ore cluster is a typical large deposit, and the ore genesis remaining controversial. The viewpoints are divided into two sides, most researchers believed that it is a SEDEX (sedimentary exhalative) type or sedimentary exhalative –reformed deposit, instead, others argue that it could be an epigenetic hydrothermal type.