首页|广东鹦鹉岭多金属矿床辉钼矿的Re-Os同位素定年及其意义

广东鹦鹉岭多金属矿床辉钼矿的Re-Os同位素定年及其意义

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通过对鹦鹉岭铜多金属矿床6件辉钼矿样品的Re-Os同位素定年,获得的模式年龄为82.96 Ma~84.75 Ma.其中1件矽卡岩型矿石中辉钼矿的187 Re-187Os模式年龄为82.96 Ma±1.2 Ma,5件石英脉型矿石中辉钼矿的187Re-187Os模式年龄为83.78 Ma~84.75 Ma,加权平均值为84.08 Ma±0.54 Ma,对应的等时线年龄为83.0 Ma±1.7 Ma,模式年龄和等时线年龄结果在误差范围内基本一致,指示鹦鹉岭多金属矿床的成矿时限为82.96 Ma~84.75 Ma,即形成于晚白垩世.鹦鹉岭矿床辉钼矿样品的Re含量较低,表明其成矿物质主要来自于壳源.该矿床形成于燕山晚期岩石圈伸展减薄环境.
Re-Os ISOTOPIC DATING OF MOLYBDENITES FROM THE YINGWULING POLYMETALLIC DEPOSIT IN GUANGDONG PROVINCE AND ITS GEOLOGICAL SIGNIFICANCE
Six molybdenite samples are selected from the Yingwuling copper polymetallic deposit to perform the Re-Os dating.It yielded weighted average model ages of 82.96 Ma to 84.75 Ma,With a narrow range variation.It was showed that the Re-Os dating of one sample collected from skarn-type ore yielded a model age of 82.96 Ma±l.2 Ma,and five molybdenite samples collected from quartz-vein-type ore yielded model ages ranging from 83.78 Ma to 84.75 Ma,with an average of 84.08 Ma±0.54 Ma,and give an isochron age of 83.0 Ma± 1.7 Ma.Evidently,model ages are compatible with isochron age in the error within the allowable range,soit constrains the absolute age of Yingwuling copper polymetallic deposit in 82.96 Ma~84.75 Ma,namely,the Late Cretaceous is the main time for the formation of ore.The molybdenites from Yingwuling copper polymetallic deposit have a low content of Re,indicating a crustal source for ore-forming materials.It was considered that the deposit formed in the Late Yanshanian lithospheric extensional and thinning environment.

Re-Os datingmolybdeniteYingwuling polymetallic depositLate YanshanianGuangdong Province

郑伟、赵海杰、陈懋弘、徐林刚、刘建新、罗大略、胡耀国

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中国地质大学地质过程与矿产资源国家重点实验室,北京 100083

中国地质科学院矿产资源研究所,北京 100037

广东省地质建设工程集团公司,广东广州 510080

广东省地质调查院,广东广州 510080

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Re-Os同位素定年 辉钼矿 鹦鹉岭多金属矿床 燕山晚期 广东

国家自然科学基金中国地质调查局地质调查项目国家重点基础研究发展规划(973计划)

4093041912120111208312012CB416704

2013

矿物岩石
四川省矿物岩石地球化学学会 成都理工大学

矿物岩石

CSTPCDCSCD北大核心
影响因子:0.8
ISSN:1001-6872
年,卷(期):2013.33(3)
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