摘要
纳日贡玛斑岩铜矿,矿体主要赋存在喜山期花岗斑岩体中.笔者通过野外观察和室内研究,从矿床地质特征,岩石地球化学特征等方面对矿床的成因进行了探讨,初步认为它是一个典型的斑岩型铜(钼)矿床.
Narigongma porphyry copper-molybdenum deposit locates in Zaduo county ,Qinghai province.The orebody is mainly in the granite-porphyry of Xishan times. By field observation and indoor study, according to the geological characters of deposit and rock geochemistry, the author discusses the origin of the deposif, and initially considers it as a typical porphyry copper-molybdenum deposit.
出处
《新疆地质》
CAS
CSCD
2007年第2期199-203,共5页
Xinjiang Geology
基金
国家973项目(2002CB412607)
中国地质调查局地质大调查项目(1212010530203)共同资助
关键词
纳日贡玛
斑岩铜(钼)矿
矿床地质特征
岩石化学特征
矿床成因
Narigongma
porphyry copper-molybdenum
deposit geological character
rock geochemistry
deposit origin
