Fluorite deposits in China: Geological features, metallogenic regularity, and research progress

被引:0
|
作者
Bei-bei Han [1 ]
Peng-qiang Shang [1 ]
Yong-zhang Gao [2 ]
Sen Jiao [1 ]
Chao-mei Yao [1 ]
Hao Zou [3 ,4 ]
Min Li [3 ,4 ]
Liang Wang [5 ]
Hou-yi Zheng [1 ]
机构
[1] China Chemical Geology and Mine Bureau
[2] Sinosteel Mining Co., Ltd.
[3] College of Earth Sciences, Chengdu University of Technology
[4] Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Natural Resources
[5] School of Earth Sciences and Resources, China University of Geosciences
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中图分类号
P619.215 [];
学科分类号
摘要
Fluorite is one of the important mineral raw materials in the industry. In China, it is mainly distributed in the provinces and regions such as Hunan, Zhejiang, Jiangxi, Inner Mongolia, Fujian, and Henan provinces,boasting huge reserves and large numbers of deposits. However, most of the fluorite deposits are on a small or medium scale. The main fluorite deposits in China were studied in this paper. Their geological features and metallogenic regularity were summarized and compared. Meanwhile, based on their main genetic factors including metallogenic fluid sources and main metallogenic geological processes, they were divided into two groups, namely meso-epithermal deposits and magmatic-hydrothermal deposits.Furthermore, based on the prospecting achievements and research progress obtained in fluorite deposits in recent years, prospecting potential predictions were made for the metallogenic prospect areas and major prospecting areas of fluorite in China. This aims to provide a theoretical basis and direction for future fluorite prospecting in China.
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页码:473 / 489
页数:17
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