德兴地区金矿成矿地质特征及找矿方向  

METALLOGENIC CHARACTERISTICS AND PROSPECTING DIRECTIONS OF GOLD DEPOSITS IN DEXING ARAE,JIANGXI

作　　者：谢代强[1] 熊文亮[1] 

机构地区：[1]江西地质矿产调查研究大队

出　　处：《贵金属地质》1997年第4期288-295,共8页

摘　　要：德兴－铜厂岩块地层序列属怀玉地体构造沉积区．金矿赋存于中元古界韩源组．控矿构造为北东东向韧性剪切带及顺层滑脱碎裂岩带．矿石类型为蚀变糜棱岩型和石英脉型．韧性剪切强应变岩带且叠加碎裂化部位是找矿的有利地段．he stratigraphic sequences of DexingTongchang block belong to the tectonosedimentary domains of Huaiyu terraneGold deposits occur in Hanyuan formation of Midde ProterozoicThe orecontrolling structure is NEEtrending ductile shear zone and superimposed layerslipping cataclastic zoneThe main types of ores are altered mylonitic and quartz vein onesThe favourable prospecting districts are the strong strain ductile shear zones which are superimposed by cataclasting

关 键 词：金矿床 成矿 地质特征 找矿方向 

分 类 号：P618.510.2[天文地球—矿床学] P618.510.8[天文地球—地质学]