摘要
本文结合矿区最新勘查成果,从成矿背景、物质来源、矿化特征等方面揭示了矿区具有较好的成矿地质条件和矿化信息。笔者通过疏理决定矿区找矿方向的关键环节,提出矿区斑岩体的侵入方向与区域NE向构造-岩浆带一致,主导矿区富碱斑岩带总体呈NE向展布并由NW向SE侵入的认识,进一步调整了找矿思路。并分析展现了矿区具有寻找大型-超大型斑岩铜钼矿床的前景,对区域喜山期富碱斑岩带的地质找矿工作具有一定的启示作用。
In combination with the newest exploration achievements,this paper deals with the Xiaolongtan poyphyry Cu-Mo ore district in the aspects of ore-forming background,material sources and mineralization characteristics and,on such a basis,points out that there exist fairly favorable geological conditions and mineralization information in the ore district.Based on organizing various kinds of metallogenic information,the authors determined the key link for ore-prospecting work in the ore district,and pointed out that there exists the consistency between the invading direction of the porphyry body in the ore district and the NE-trending tectonic-magmatic belt,and that the major alkali-rich porphyry belt in the ore district assumes NE-trending distribution and invaded from northwest to southeast,thus readjusting the train of thought for ore-prospecting.The authors also indicate through analysis that there exists the possibility of finding large-superlarge porphyry Cu-Mo deposits in the ore district.The results obtained by the authors play some instructive role in search for mineral deposits in regional Himalayan period alkali-rich porphyry belt.
作者
张金学
刘利超
陈梁
郭桂林
罗洪昌
戚林坤
ZHANG Jin-xue;LIU Li-chao;CHEN Liang;GUO Gui-lin;LUO Hong-chang;QI Lin-kun(No.310 Geological Party,Yunnan Nonferrous Metals Geological Bureau,Dali,Yunnan 671000)
出处
《地球学报》
CAS
CSCD
北大核心
2013年第S01期95-100,共6页
Acta Geoscientica Sinica
基金
云南省三年找矿行动计划祥云马厂箐—宾川小龙潭金铜钼多金属矿整装勘查项目“云南省宾川县小龙潭斑岩铜钼矿普查”(编号:201100024)资助。
关键词
构造-岩浆带
喜山期富碱斑岩
斑岩铜钼矿
找矿思路
前景
tectonic-magmatic belt
alkali-rich porphyry of Himalayan period
porphyry Cu-Mo deposit
train of thought for ore-prospecting work
prospect