首页|钦杭成矿带南段旗鼓岭铜钨钼多金属矿床的辉钼矿Re-Os同位素年龄及成矿物质来源

钦杭成矿带南段旗鼓岭铜钨钼多金属矿床的辉钼矿Re-Os同位素年龄及成矿物质来源

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  • 国家科技期刊平台
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广东旗鼓岭铜钨钼多金属矿是近年来在云开地区新发现且具有重要找矿远景的矿床之一.矿体形态不规则,主要呈层状、似层状和透镜状产出在矽卡岩中.本文在详细了解矿床地质特征的基础上,通过辉钼矿Re-Os同位素定年技术首次对旗鼓岭矿床进行了成矿时代的厘定.5件辉钼矿样品的模式年龄为163.6～165.3Ma,加权平均年龄为164.54±0.94 Ma,表明旗鼓岭铜钨钼多金属矿床成矿作用发生于中侏罗世晚期.该矿床辉钼矿样品的Re含量变化于76.86～86.22 μg/g之间,表明其成矿物质具有壳幔混源的特征.黄铁矿的δ34 S组成范围比较窄,变化范围为1.4‰～2.5‰,显示来自于岩浆热液.旗鼓岭铜钨钼多金属矿床成矿年龄的厘定为下一步在区内开展150～170Ma左右的斑岩-矽卡岩多金属矿床找矿勘探提供了重要的线索,也标志着著名的钦杭成矿带进一步向南延伸,同时为进一步深入研究钦杭成矿带成岩成矿作用提供了新的资料和证据.
Re-Os Age of Molybdenite and Ore-Forming Material Source of the Qiguling Cu-W-Mo Polymetallic Deposit in the Southern Section of the Qinghang Metallogenic Belt
The Qiguling Cu-W-Mo polymetallic deposit,located in the Yunkai area,is one of the newly discovered deposits with huge prospecting potential.The ore bodies mainly occur as lamellar,stratiods and lenses in skarn.Based on detailed geologic characteristics of the deposit,this study re determined the metallogenic time of the Qiguling deposit using molybdenite Re-Os dating technology.Precise Re-Os dating of molybdenite shows that the Re-Os model ages of five samples range from 163.6 Ma to 165.3 Ma,with a weighted mean age of 164.54± 0.94 Ma,indicating that the timing for Cu-W-Mo polymetallic mineralization formed in the late stage of the Mid-Jurassic.Rhenium content of molybdenum in the samples ranges from 76.86～86.22 μg/g,and this indicates the ore-forming material is characterized by crust and mantle mixing in origin.δ34S values of pyrites of this deposit have a narrow range of 1.4‰ ～ 2.5‰,showing magmatic sulfur.Determination of metallogenic time for the Qiguling Cu-W-Mo deposit not only provides an important clue to future prospecting for 150～170 Ma porphyry-skarn Cu polymetallic deposits in this area,but also marks the southward extension of the well-known Qinhang metallogenic belt.Therefore,this study offers new information for further research of diagenesis and metallogenesis of the Qinhang metallogenic belt.

Qiguling Cu-W-Mo polymetallic depositmolybdenite Re-Os datingsources of ore-forming materialsYunkai areathe Qinhang metallogenic belt

郑伟、欧阳志侠、陈友良、赵海杰、刘东宏、吴晓东、杨胜虎、汪汝澎、楚克磊

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中国地质科学院矿产资源研究所,国土资源部成矿作用与资源评价重点实验室,北京,100037

广东省有色金属地质局,广州,510080

成都理工大学地球科学学院,成都,610059

中国地质科学院,北京,100037

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旗鼓岭铜多金属矿 辉钼矿Re-Os定年 成矿物质来源 云开地区 钦杭成矿带

国家重点研发计划项目国家自然科学基金中国博士后科学基金中国地质调查局地质调查工作项目中国地质调查局地质调查工作项目

2017YFC0601403417020832017M610105121201140158011212011120826

2018

地质学报
中国地质学会

地质学报

CSTPCDCSCD北大核心EI
影响因子：2.17
ISSN：0001-5717
年,卷(期)：2018.92(1)
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