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Geochemical Characteristics of Calcite and Its Significance in Sanqisan Uranium Deposit
Author(s) -
XU Zhengqi,
ZHANG Guodong,
LI Ping,
SONG Hao,
WANG Ye
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 - 10.1111/1755-6724.12381_37
Subject(s) - china , ping (video games) , chinese academy of sciences , geography , geology , geochemistry , library science , archaeology , computer science , computer security
The Sanqisan uranium deposits are located in the western part of the geologic region known as the Youjiang basin, the north end of Xidaming Mountain convex and the North east end of Naling-Fengtun anticline of Daxin concave broken bunch. This deposit is a typical carbonatesiliceous-pelitic rock type uranium deposit in South China. Controlled by tectonic fracture zone, the orebodies occur in the carbonate rock and clastic rock in Devonian. It is controversial in the source of ore-forming fluid for a long time. The calcite samples are collected to study the oreforming fluid of the Sanqisan uranium deposits, by the geochemical study on the the trace elements, rare earth elements and isotope.