大冶毛铺～阳新两剑桥断裂带东段找矿方向  

ORE SEARCHING DIRECTION IN THE EASTERN SECTION OF DAYE MAOPU～YANGXIN LIANGJIANQIAO FRACTURE ZONE

作　　者：黄智辉[1] 孙四权[1] 陈前军[1] 

机构地区：[1]鄂东南地质大队,湖北大冶435100

出　　处：《资源环境与工程》2006年第3期221-226,259,共7页Resources Environment & Engineering

摘　　要：通过大冶毛铺～阳新两剑桥东西向断裂带东段地质背景、已知矿床地质特征及前人地质工作的综合分析，结合西段已知矿床的特征和鸡冠嘴铜金矿床成功的找矿经验，分析东西向断裂带的东段与阳新火山岩沉积盆地边缘交汇地段存在大量的隐伏斑岩型铜钼金矿床的找矿信息，推断阳新火山岩沉积盆地边缘存在隐伏含铜钼金成矿岩体。According to the geological background of the eastern section of Daye MaoFu～Yangxin Liangjianqiao fracture zone, the characters of the known mineral deposits and the comprehensive analysis of the previous geologic work, and in combination of the characters of the known mineral deposits in the western section and the successful ore searching experience of Jiguanzui copper - gold deposit, this paper analyses that there is large amount of ore searching information of hidden porphyry copper - molybdenum - gold deposit in the place where the eastern section of the east - west fracture zone and the edge of Yangxin volcanic - rock sedimentary basin intersect, and infers that there occurs the copper - molybdenum - gold ore - forming massif at the edge of Yangxin volcanic - rock sedimentary basin.

关 键 词：断裂带东段 火山盆地边缘 隐伏矿床 

分 类 号：P588.13[天文地球—岩石学] P612[天文地球—地质学]