Analysis of Geological Characteristics and Metallogenic Model of Hukeng Tungsten Deposit in Jiangxi Province
作者: 余驰达 ：东华理工大学，江西 南昌;
Abstract: Hukeng tungsten deposit is the large black tungsten quartz-vein-type deposit, which is located in Wugong mountain mineralization belt in the central part of Jiangxi province, distributed in the southern edge of Qing Wan Longshan Massif and penetrated in the sinian Tiger Tong group formation. The exposed area is 14 km2. Different from the typical “five stories” mode, the deposite veins were concentrated in contact with rock. Besides general block structure, there is also common banded structure in the Ore-bearing quartz veins. Detailed field catalogs and microscopic studies have shown that banded quartz vein is the ductile shear zone, characterized by the newborn penetrative foliation and lines. Petrological studies indicate that banded ore belongs to quartz mylonite and its microstructure characteristic is the rich plastic deformation. By analyzing the mine vein occurrence, shape, size and its relationship to construct and rock, the vein occurrence is summed up, and it also demonstrates that the deep veins of contacts lean to south and southern translation, characterized by fewer in eastern and northern ,more in western and southern, which indicates the emphasis on prospecting should be in the deep Southwest.
文章引用: 余驰达 (2015) 江西浒坑钨矿地质特征及成矿模式分析。 自然科学， 3， 121-126. doi: 10.12677/OJNS.2015.34016
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