内蒙乌奴格吐山斑岩铜钼矿床地质及深部预测  

CORRELATION BETWEEN THE NORTHERN SOUTHERN ORE SECTIONS IN WUNUGETUSHAN PORPHYRY COPPER DEPOSIT, INNER MONGOLIA, CHINA

作　　者：金力夫 孙凤兴[2] 

机构地区：[1]黑龙江冶金地质研究所 [2]长春地质学院

出　　处：《长春地质学院学报》1990年第1期61-67,共7页

摘　　要：本文通过矿床地质特点的分析研究,应用数学地质方法、对前人已取得的各种岩、矿测试数据进行了统计分析,并结合剥蚀程度的研究,做了南、北两个矿段之间的综合分析对比,进一步探讨矿区内F_7断层两侧的地层相对运动方向或升降,提出了新的认识,从而对矿床深部远景进行预测,扩大了找矿范围,为今后的勘探工程设计提供可靠依据。A post-metallogenic main fault, F7, cut and divided Wunugetushan porphyry copper diposit into two sections, the northern and southern sections. Through the geological correlation between the two sections, including denudation depths, metallogenic temperatures, mineralizations, shapes, inclusions, trace elements and anomalous geochemistries of the ore bodies as well as their country rocks, the authors made a conclusion that the south zone has a relative subsidence due to the F fault activi ty. Meanwhile, the authors also made a throrogh investigation on prognosis of mineral deposits in the deep pert of crust, providing some available information for propecting of ore deposits.

关 键 词：内蒙 斑岩 铜矿 钼矿 地质 预测 

分 类 号：P618.410.2[天文地球—矿床学]