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Hydrothermal Sedimentary Mineralization of the Super‐large Bamianshan Fluorite Deposit in Zhejiang Province, China
Author(s) -
Yuchuan HAN,
Xuehui XIA,
Siyu PANG,
Shaokang XU
Publication year - 2012
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/j.1755-6724.2012.00701.x
Subject(s) - fluorite , geology , geochemistry , hydrothermal circulation , mineralization (soil science) , sedimentary rock , tectonics , ore genesis , fluid inclusions , mineralogy , chemistry , paleontology , soil water , organic chemistry , soil science
The Bamianshan fluorite deposit is a super‐large one recently discovered in Zhejiang Province of China. This paper presents an analysis of its geological background, orebody and ore characteristics, petrochemical characteristics of host rocks, rare earth elements (REE) of rocks and ores, fluid inclusions in fluorite and Sm‐Nd isotopic features in an effort to study its sedimentary mineralization. The result shows that the super‐large Bamianshan fluorite deposit is of hydrothermal sedimentation genesis, deformed by the later hydrothermal fluid. Integrated with host rocks and orebody characteristics, it is inferred that the deposit originates from the Cambrian sedimentary rocks. And the later magmatic activities deformed some orebodies in different degrees, forming steeply dipping vein orebodies in the tectonic belts regionally.