摘要
矿区位于中生代溧阳火山盆地南西部,郎溪中生代红层盆地北侧,在东西向坳陷带和北北东向断裂带的交汇部位处,现已发现小型铜、铁矿床和多个铜铁矿化点。经过先期勘查,区内已圈定铜矿体3个,矿体平面形态为S形,矿体主要赋存于北北东断裂中,产状与断裂一致。矿石有益组分主要为铜、铁、铅、锌、金等。在铜官山矿床外围及深部具有较好的找矿潜力,铜铁矿找矿潜力较大。
The mine is located in the southern west of Mesozoic volcanic basin in Liyang, and in the north of Mesozoic red bed basin in Langxi. At intersections of the east - west depression and NNE - trending fault zone, a small scale of copper, iron ore deposits and a number of copper and iron mineralization were found. After a preliminary investigation, in the area 3 copper ore deposits were delineated, the ore deposits in morphology are S shaped , mainly occur in the NNE - trending fault zone, their occurrence is consistent with the Main useful components in the ore are copper, iron, lead, zinc, gold, etc. In the peripheral and Tongguanshan deposits prospecting is potential, and copper ore prospecting potential is big. fault strike. deep parts of
出处
《安徽理工大学学报（自然科学版）》
CAS
2013年第4期67-71,共5页
Journal of Anhui University of Science and Technology:Natural Science
关键词
铜(铁)矿
地质特征
找矿方向
copper（iron） ore
geological features
prospecting direction
