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Geochemical Characteristics of Trace Element of Calcite, Quartz of the No. 510‐1 Uranium Ore Deposit in Zoige
Author(s) -
HE Zhongxiang,
CHEN Youliang,
CHANG Dan,
WEI Jia,
HU Xugang
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 - 10.1111/1755-6724.12379_22
Subject(s) - nuclear technology , geology , library science , mining engineering , computer science , physics , nuclear power , nuclear physics
one of the famous carbonaceous-siliceous-argillitic rock uranium deposit producing districts in China, The No.5101 uranium deposit is one of the typical desposits that have representative significance in this district, ore mineral assemblages of the deposit often forms the combination of pitchblende, pyrite, calcite, quartz, which reflects that hydrothermal minerals such as calcite, quartz and pyrite are closely related with uranium mineralization(Chen Youliang et al., 2012). The characteristics of trace elements geochemical of hydrothermal minerals such as calcite, quartz and pyrite in this uranium deposit are studied in order to provide important information for the sources and evolution of ore-forming fluid in this dissertation.