摘要
江西德兴银山铜多金属矿深部勘探项目取得重要勘查成果,新探明储量(331+332+333)铜54万t,铅+锌23万t,金57 t,银914 t,硫593万t。为进一步扩大银山深部找矿远景,评价矿区更深部位的找矿潜力和预测赋矿有利空间,根据本次深部勘探各类探矿工程的详细地质观察编录,结合岩矿试验工作,进一步系统总结勘探报告的成果,分析研究矿床基础地质条件和成矿特征,依此提炼获得新的认识。研究表明:(1)燕山期银山次火山岩体与成矿密切相关,3#英安斑岩与铜金成矿有关,5#石英斑岩与铅锌银矿化有关;(2)银山背斜北西翼控制了绝大多数矿体的产出和分布;(3)矿体的定位和形态受主断裂及其两侧伴生的网状裂隙组成的断裂构造带控制,细网脉浸染状矿石为主要矿化类型;(4)与铜矿化、铅锌矿化相伴生的热液蚀变分别是以硅化绢云母化和绿泥石化碳酸盐化为主的低温蚀变组合。银山铜多金属矿深部矿体尚未封闭,在银山九区—西山区深部是后续找矿的最佳方向。
The deep exploration project of Yinshan copper polymetallic mine in Dexing,Jiangxi Province undertaken by Jiangxi No.4 Nonferrous Geological Exploration Team has achieved important exploration results.The newly proved resource reserves(331+332+333)are 540000 tons of copper,230000 tons of lead+zinc,57 tons of gold,914 tons of silver and 5.93 million tons of sulfur.It is equal to increasing the scale of a large copper mine,a large gold mine,a medium-sized lead-zinc mine and a near large silver mine.In this deep exploration,the original geological logging of more than 100000 meters of drilling and more than 17000 meters of tunnel has been carried out.35900 basic analysis samples have been taken and various rock and ore test samples matching with the exploration stage have been sent for inspection.In order to further expand the prospecting in the deep part of Yinshan,evaluate the prospecting potential in the deeper part of the mining area and predict the favorable space for ore generation,through the detailed geological observation and recording of various prospecting projects in the deep exploration,combined with the rock and ore test work,further systematically summarize the results of the exploration report,analyze and study the basic geological conditions and metallogenic characteristics of the deposit formation,so as to extract the results.The new understanding includes:(1)Yanshanian Yinshan subvolcanic body is closely related to mineralization,3#dacite porphyry is related to copper gold mineralization,5#quartz porphyry is related to lead zinc silver mineralization.(2)The altered quartz diorite in Caledonian period appears in many places on the outer side of the 3 Ying’an porphyry in Jiutong district,which,together with sericite phyllite and blasting breccia,forms the ore bearing surrounding rock in the Ninth-Xishan district.The opened magmatic activity channel is favorable for the emplacement of the 3 rock body related to the mineralization in Yanshan period.(3)The two flanks of Yinshan anticline are associated with the fracture structure belt,which is the main ore controlling structure.The northwest wing is associated with the East-West fracture structure belt,which is extremely developed with a wide strike and a long extension length.The south-east wing develops the North-South fracture structure belt,which is characterized by a short strike and a scattered distribution,which results in the north-west wing of Yinshan anticline controlling the occurrence and distribution of most ore bodies.(4)The location and shape of the orebody are directly controlled by the main fault and its associated network fractures on both sides.The sulfide vein continuity in the main fault controls the continuity of the ore body.The fine network vein ore is the main mineralization type,and the thick and large ore bodies are often composed of several main fault surfaces close to each other,such as the Ninth-Xishan District copper ore body.(5)The hydrothermal alteration associated with mineralization is a low-temperature alteration combination mainly composed of sericitization,carbonation and chloritization,which is lack of high-temperature potassium silicate salinization of porphyry deposits.The deep orebody of Yinshan copper polymetallic mine has not been closed,especially the outer contact zone on both sides of the deep 3 Ying’an porphyry at the turning part of Yinshan Ninth-Xishan area and the deep part of known orebody inclined extension are the best direction for subsequent ore prospecting.
作者
胡金山
胡福林
刘金刚
李宁
胡国柳
王国光
HU Jinshan;HU Fulin;LIU Jingang;LI Ning;HU Guoliu;WANG Guoguang(No.4 Team,Jiangxi Bureau of Nonferrous Metal Geoexploration,Jingdezhen 333001,Jiangxi,China;State Key Laboratory for Mineral Deposits Research,School of Earth Sciences and Engineering,Institute of Geofluids,Nanjing University,Nanjing 210023,Jiangsu,China)
出处
《黄金科学技术》
CSCD
2020年第5期688-700,共13页
Gold Science and Technology
基金
国家自然科学基金面上项目“江西德兴斑岩铜(钼)矿田矿石矿物和共生脉石矿物的流体包裹体对比研究”(编号:41772063)
江西省有色地质勘查四队项目“江西省德兴市银山矿区铜铅锌矿勘探”联合资助
关键词
深部找矿
成矿特征
找矿方向
银山铜多金属矿
德兴
江西省
deep prospecting
mineralization characteristics
prospecting direction
Yinshan copper polymetallic ore
Dexing
Jiangxi Province
