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西藏申扎县舍索铜多金属矿床辉钼矿Re-Os年代学及地质意义
引用本文:赵元艺. 西藏申扎县舍索铜多金属矿床辉钼矿Re-Os年代学及地质意义[J]. 地质学报, 2009, 83(8): 1150-1158
作者姓名:赵元艺
作者单位:中国地质科学院矿产资源研究所
基金项目:国家科技支撑课题《西藏班公湖岛弧带铜、金、富铁矿评价与综合找矿技术方法示范研究》(编号: 2006BAB01A05)之专题《区域成矿模型与典型矿床成因模型研究》与地质调查项目《西藏班公湖-怒江成矿带找矿远景区评价》
摘    要:舍索铜多金属矿床位于西藏申扎县雄梅乡政府所在地南4km处。为现今在冈底斯北麓正在开采的少数矽卡岩型铜矿床之一。由辉钼矿测年结果可以看出,Re-Os等时线为116.2±1.9 Ma,而模式年龄的平均值为115.7±1.3 Ma。因此,舍索矿床的成矿年龄应为116 Ma,为燕山晚期的产物。其成矿年龄与冈底斯成矿带的相距较远,而与班公湖-怒江成矿带的相近,为班公湖-怒江缝合带闭合之后碰撞后阶段的产物,其成矿物源与壳源关系更为密切。

关 键 词:Re-Os等时线,辉钼矿,矽卡岩型铜多金属矿床,舍索  西藏

Re-Os Dating of Molybdenite from the Shesuo Copper Polymetallic ore in Shenzha County, Tibet and Its Geological Significance
zhao yuanyi. Re-Os Dating of Molybdenite from the Shesuo Copper Polymetallic ore in Shenzha County, Tibet and Its Geological Significance[J]. Acta Geologica Sinica, 2009, 83(8): 1150-1158
Authors:zhao yuanyi
Affiliation:Institute of Mineral Resources, CAGS
Abstract:Shesuo copper polymetallic ore deposit is located in 4km of south of Xiongmei town, Shenzha county, Tibet. It is one of several deposits, located in the north part of Gangdese ore belt, that is exploring at present .The age of Re-Os isotime line from molybdenite is 116.2±1.9 Ma. The average age of model is 115.7±1.3 Ma.Therefore the age of Shesuo copper polymetallic ore deposit is 116 Ma.It is the late of Yanshan epoch . It is obviously different with that of Gangdesi ore belt,but near that of Bangong Co-Nujiang belt.So this deposit is the result of postcollision of Bangong Co-Nujiang belt.Ore-forming material of it is closely related to the crust.
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