摘要
那陵格勒含矿斑岩带位于秦祁昆中央造山带东昆仑中段,其中有多个斑岩铜(钼-金)矿床产出。含矿斑岩与三叠纪花岗岩密切共生。笔者对该带斑岩多金属铜矿床构造背景、蚀变与矿化关系、地球化学特征及含矿斑岩的岩石学成因进行了初步研究。
Nalenggele ore-bearing porphyry zone is located at the east Qinling-Qilian-Kunlun orogenic belt and includes a number of porphyry Cu(Mo-Au) deposit.Ore-bearing porphyry is close symbiosis with Triassic granite.In this paper,we will systematically research on the tectonic setting,the relationship between alteration and mineralization,geochemical characteristics,petrogenesis of porphyry Cu(Mo-Au) deposit.
出处
《西北地质》
CAS
CSCD
2010年第4期245-255,共11页
Northwestern Geology
基金
国家科技支撑计划项目(2006BAB01A01)
中国地质调查局地质大调查项目(1212010813046)资助
关键词
东昆仑
那陵格勒
斑岩铜矿
east Kunlun
Nalenggele
porphyry deposit