Analysis on Geological Characteristics and Genesis of the Yaganbuyang Fluorite Deposit in Ruoqiang County
The Yaganbuyang Fluorite Deposit is located in the central southern part of the Altun Complex,a tertiary tectonic unit in the southern part of the Azhong Block,it belongs to the Altun(massif)Fe-Cu-Ni-fluorite-asbestos-jade-muscovite-dolomite-quartzite-gypsum-coal ore belt.Fluorite mineralization is mainly distributed in the biotite plagioclase gneiss strata of a rock group of the Altun rock group on both sides of the Gaijile fault,as well as in the areas where Middle Ordovician intrusive rocks and calcite veins are developed,it is clearly controlled by factors such as strata,lithology,and faults.Preliminary research suggests that the genesis type of the deposit is a low-temperature hydrothermal filled fluorite deposit.
Yaganbuyang Fluorite Depositgeological characteristicsgenesisRuoqiang County