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Fluid Inclusions and Rare Earth Elements of the Badu Gold Deposit, Guangxi, China: Implications for Mineralization
Author(s) -
LI Peirong,
PANG Baocheng,
WANG Baohua,
LI Yuanqiang,
ZHOU Yequan,
LV Jiawen,
MA Jingjing
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_29
Subject(s) - china , chinese academy of sciences , mineralization (soil science) , geology , geochemistry , archaeology , geography , soil science , soil water
Badu gold deposit, located in the southwest of Tianlin county, Guangxi province, is a microdisseminated gold deposit occurred in Diabase. Besides, there are several other gold deposits occurred in Diabase in northwestern Guangxi. Because of these gold deposits relating to diabase intrusions spatially, some researchers called them diabase-type gold deposit (Xiao, 1997; Pan et al, 1998). There are few previous studies involving ore-forming fluids in the diabase-type deposits (Hu et al., 1995).The genesis of this type gold deposit is still unclear. Fluid inclusion and REE data in this study provide some clues to ore genesis.