Fluorite deposit type in China

The types of fluorite deposits in China are as follows:

table   Fluorite deposit type in China
Deposit type
Mineral deposit cause
Deposit and ore characteristics
Instance
Silicate fluorite deposit
This type of deposit is formed by condensing the ore-bearing hydrothermal fluid along the strata of the strata in the siliceous rocks, such as the cracks of the slurry, shale , rhyolite, granite and gneiss . Medium and low temperature hydrothermal deposit
The deposit is formed by the fluorite and its associated minerals cemented together in the fissures. Due to the various shapes of the fissures, various ore bodies are formed, generally in the form of veins, nets, dendrites, sacs, and lentils. Wait. Some ores, strips, breccias or clusters of ore. The main mineral deposit is fluorite, fluorite closely associated minerals are quartz, as well as a small amount of calcite, pyrite, kaolin. The massive fluorite crystal particles are relatively coarse, ranging from a few millimeters to tens of millimeters. Fluorite embedded in quartz, such as veins or mesh, has extremely uneven particle size, and the thickness is only 0.01 to 0.02 mm, and is generally 0.05 to 0.6 mm. This type of fluorite deposit has a high content of calcium fluoride in fluorite, generally up to 70% to 80%.
Zhejiang Dongfeng Fluorite Mine, Hubei Hong'an Fluorite Mine, Henan Minggang Fluorite Mine, Inner Mongolia Huade County Fluorite Mine, Tongbai Fluorite Mine
Carbonate fluorite deposit
This type of deposit is a fluorinated hydrothermal fluid immersed in the limestone rock fissure and formed by the interaction with limestone.
This type of deposit has a complex and diverse ore shape, which is vein-like, cystic, lenticular, strip-shaped, disseminated or more regular. The main mineral fluorite is densely packed, breccia or disseminated. There are many symbiotic minerals, such as calcite, quartz and barite . Calcium fluoride content is generally below 65%
Jiangxi Dean fluorite mine
Multi-metal fluorite deposit
This type of deposit has many genesis, and the fluorite generation time is between the late to the middle of the skarn, which is a medium temperature hydrothermal filling deposit.
The fluorite and quartz type deposit filled with a large number of crushing zone, were breccia plastic structure, generally rough grain, a small amount of the form of fine veins, with the main mineral fluorite galena, sphalerite, copper ore yellow, yellow Metal minerals such as iron ore are symbiotic. Non-metallic minerals are quartz, barite, sericite, chlorite, kaolin. The fluorite crystal particles are generally 20 to 30 mm and up to 75 mm. Fluorite content is 14% to 16%
Hunan Taolin Lead-Zinc Mine
Note: China's single fluorite deposit generally has the following characteristics:
(1) The deposits are generally rich and poor, and the upper and lower are small; (2) the points are small and the distribution is uneven, the East China points are large, the quantity is large, the central and southern points are small, the quantity is large, the northeast is poor, and the southwest is less; 3) The ore body is vein-like, with steep slope output, and most of it needs underground mining; (4) The ore structure is mainly blocky, breccia and strip. The lump ore is rich in ore, the breccia is lean, and the strip is easy to choose.

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