中条山地区郭家沟基性-超基性岩LA-ICP-MS锆石U-Pb年代学及地质意义
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摘要
中条山地区地层主要由涑水片麻杂岩、绛县群、中条群、担山石群和熊耳群组成,该区发育著名的铜矿峪型矿床、胡-篦型矿床和横岭关型矿床。中条山地区郭家沟基性-超基性岩主要侵位涑水片麻杂岩中,岩体由内向外发育透闪岩-变余辉石岩-辉长岩-斜长角闪岩的岩相分带。透闪岩LA-ICP-MS锆石U-Pb显示岩体侵位于2303Ma,属于古元古代。通过岩体野外侵位、覆盖关系,结合已有同位素资料,认为绛县群横岭关亚群沉积时限在2189Ma～2303Ma之间。同时根据岩体构造环境、岩体形态、岩相分带、铜矿化情况,以及铜凹组和篦子沟组两套含矿地层中均出现本期岩浆锆石,认为本区基性-超级性岩中发育有铜成矿作用,找矿前景乐观。
The Zhongtiao Mountain consists mainly of the Sushui gneiss complex,Jiangxian group,Zhongtiao group,Dhanshanshi group and Xiong'er group,which developed Tongkuangyu type copper deposit,Hu-Bi type copper deposit and Henglingguan type copper deposit. The main emplacement of the Guojiagou basic-ultrabasic rocks is the Sushui gneiss complex,and the intrusion with lithological zoning,from the core to the edge,is tremolite-palimpsest pyroxenolite-gabbro-amphibolite. LA-ICP-MS zircon U-Pb of tremolite shows intrusion of rock mass in 2303 Ma,which is a Paleoproterozoic age. Through the field emplacement and coverage of rock mass,combined with isotopic data,we believe that the Hanglingguan subgroup was formed at 2189 ～ 2303 Ma. According to the tectonic setting,shape,lithological zoning and copper mineralization,and both Tongwa Formation and Bizigou Formation,which are two ore-bearing strata,have detrital zircons that from Guojiagou basic-ultrabasic rock,indicating the Guojiagou basic-ultrabasic rocks have copper mineralization,with optimistic ore-potential.
The Zhongtiao Mountain consists mainly of the Sushui gneiss complex,Jiangxian group,Zhongtiao group,Dhanshanshi group and Xiong'er group,which developed Tongkuangyu type copper deposit,Hu-Bi type copper deposit and Henglingguan type copper deposit. The main emplacement of the Guojiagou basic-ultrabasic rocks is the Sushui gneiss complex,and the intrusion with lithological zoning,from the core to the edge,is tremolite-palimpsest pyroxenolite-gabbro-amphibolite. LA-ICP-MS zircon U-Pb of tremolite shows intrusion of rock mass in 2303 Ma,which is a Paleoproterozoic age. Through the field emplacement and coverage of rock mass,combined with isotopic data,we believe that the Hanglingguan subgroup was formed at 2189 ～ 2303 Ma. According to the tectonic setting,shape,lithological zoning and copper mineralization,and both Tongwa Formation and Bizigou Formation,which are two ore-bearing strata,have detrital zircons that from Guojiagou basic-ultrabasic rock,indicating the Guojiagou basic-ultrabasic rocks have copper mineralization,with optimistic ore-potential.
引文
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