摘要
西藏甲玛铜多金属矿床中辉钼矿是主要的矿石矿物,普遍发育,产出于不同的矿石类型(角岩型、矽卡岩型、斑岩型)矿石中。辉钼矿大多分布于裂隙、节理面上和石英脉或不同岩性岩石中。矽卡岩型矿石中辉钼矿呈微细粒浸染状、团斑状、脉状等,直接分布于矽卡岩中或矽卡岩中后期的石英脉中。采集西藏甲玛铜多金属矿床矽卡岩型矿石中不同产状的辉钼矿,进行铼-锇同位素测年,得到等时线年龄为(15.34±0.10)Ma,模式年龄变化于(15.21±0.22)Ma～(15.50±0.22)Ma,说明甲玛的辉钼矿成矿年龄集中在15Ma左右。结合前人的年代学研究成果,认为甲玛铜多金属矿成矿时代与冈底斯斑岩铜矿带斑岩铜矿的成矿年龄相近,可以否定甲玛铜多金属矿海底喷流沉积成矿成因的观点,为甲玛铜多金属矿的成矿成因和斑岩-矽卡岩型矿体的深部找矿提供了理论依据。
Different molybdenites were collected from the Jiama copper polymetallic deposit for Re-Os isotopic dating. The isochron age of （15.34±0. 10） Ma, and model age of （15.21 ±0.22） Ma- （15.50±0.22） Ma were obtained. This results are similar to the data from the previous Re-Os dating results, which indicates that the mineralization age of molybdenites in Jiama is around 15 Ma. According to Re-Os dating results of other molybdenite from porphyry copper deposits in Gangdese belt, which is considered to have the similar mineralization age with that of the Jiama copper polymetallic deposit, it provides a reference for further study on geological genesis of the Jiama copper polymetallic deposit and a theoretical basis for deep earth prospecting of porphyry-skam ore bodies.
出处
《岩矿测试》
CAS
CSCD
北大核心
2009年第3期265-268,共4页
Rock and Mineral Analysis
基金
技术开发项目--西藏墨竹工卡县甲玛铜多金属矿床地质特征及找矿方向研究项目资助(E0804)
国土资源地质大调查项目资助(1212010633903)
关键词
甲玛铜多金属矿
辉钼矿
铼-锇同位素定年
成矿特征
the Jiama copper polymetallic deposit
molybdenite
Re-Os isotopic dating
mineralization characteristics
