江西省赣县黄婆地钨多金属矿矿床地质特征.pdfVIP

Advances in Geosciences 地球科学前沿, 2016, 6(6), 490-498 Published Online December 2016 in Hans. /journal/ag /10.12677/ag.2016.66052 Geological Characteristics of Huangpodi Tungsten Polymetal Mine, Ganxian in Jiangxi Jianping Luo, Rensheng Liu Nuclear Industry Geological Bureau of Jiangxi Province, Ganzhou Jiangxi th th th Received: Dec. 8 , 2016; accepted: Dec. 26 , 2016; published: Dec. 29 , 2016 Copyright © 2016 by authors and Hans Publishers Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). /licenses/by/4.0/ Open Access Abstract Huangpodi tungsten polymetal mining area is located in the joint position of Yushan tectonic belt, NE, to Chongyi—Huichang tectonic belt, EW. Magmatic activity is frequent in this area; fold and fault also have good development. The research of the stratal, tectonic, magmatic and other data of Huangpodi tungsten polymetal mining area shows that the orebody mainly occurs in the sandstone, fine sand- stone of lower Carboniferous Zishan formation and near the contact zone with the granite. There are two orebody types: one is skarn scheelite polymetallic orebody; another is quartz vein wolframite orebody. The layered skarn type orebody is the main body of mining at present. Keywords Tungsten-Zinc Ore, Geological Characteristics, Huangpodi 江西省赣县黄婆地钨多金属矿矿床地质特征 罗建平，刘仁生 江西省核工业地质局，江西 赣州 收稿日期：2016年12月8 日；录用日期：2016年12月26 日；发布日期：2016年12月29 日 摘 要 黄婆地钨多金属矿矿区位于北东向于山构造带与东西向崇义—会昌构造带的交汇部位。区内岩浆活动强 文章引用: 罗建平, 刘仁生. 江西省赣县黄婆地钨多金属矿矿床地质特征[J]. 地球科学前沿, 2016, 6(6): 490-498. /10.12677/ag.2016.66052 罗建平，刘仁生 烈而频繁，褶皱、断烈构造较发育。通过对黄婆地钨多金属矿区的地