Geological Characteristics and Metallogenic Rules of Wanghuayuan Copper Mine, Ningdu Jiangxi
Abstract: Wanghuayuan copper polymetallic ore lies in the northern part of mining area, located in the Eurasian continental plate and the Pacific plate west coast mansion inside the reduction plate, and has experienced Yanshan multi-stage magmatic activity. With combination of the Strati- graphic, structural and magmatic rocks of Wanghuayuan copper polymetallic mining area, it summarizes what Copper polymetallic ore is mainly produced in the Wanghuayuan granite rock and near the contact zone of Sinian metamorphic granite, orebody is controlled by NE trending quartz veins and the near ore greisenized. According to mineral assemblages and ore bed mineral generation sequence analysis. There are three stages of mineral generation in the Wanghuayuan mining area: early stage of high and medium temperature, late stage at low tem- perature and the secondary phase. By comparing with the metallogenic regularity of copper polymetallic deposit in the area, it can be speculated that the scope of prospecting which is about 1.5 square kilometers around the mine lot has good mineralization and discovery prospects.
文章引用: 刘仁生 , 邹东风 , 刘 茜 (2014) 江西省宁都县王花沅铜多金属矿床地质特征与成矿规律。 地球科学前沿， 4， 294-301. doi: 10.12677/AG.2014.44036
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