文章摘要
卫晓锋,阴元军,毛启贵,吕晓强,朱江建,张建斌,程志龙.东天山西凤山金矿花岗岩锆石U-Pb年龄、地球化学及其对成岩成矿时代的限定[J].矿产勘查,2020,11(10):2072-2086
东天山西凤山金矿花岗岩锆石U-Pb年龄、地球化学及其对成岩成矿时代的限定
Zircon U-Pb geochronology and petrogeochemistry of granitic rocks of the Xifengshan gold deposit in eastern Tianshan and limitation on diagenesis and mineralization times
投稿时间:2019-12-01  
DOI:10.1016/j.jseses.05.011.
中文关键词: 金矿  锆石U-Pb年龄  地球化学  成矿成岩关系  西凤山  东天山
英文关键词: gold deposit, zircon U-Pb age,geochemically,metallogenic characteristics,Xifengshan deposit, eastern Tianshan
基金项目:中国地质调查局项目(编号:121201001000150010)资助。
作者单位E-mail
卫晓锋 北京矿产地质研究院有限责任公司,北京 100012  
阴元军 中色地科矿产勘查股份有限公司,北京 100012 854938700@qq.com 
毛启贵 北京矿产地质研究院有限责任公司,北京 100012  
吕晓强 北京矿产地质研究院有限责任公司,北京 100012  
朱江建 北京矿产地质研究院有限责任公司,北京 100012  
张建斌 北京矿产地质研究院有限责任公司,北京 100012  
程志龙 北京矿产地质研究院有限责任公司,北京 100012  
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中文摘要:
      为探讨西凤山金矿岩浆活动与成矿作用关系,对赋矿花岗岩类岩体(脉)(花岗岩、花岗斑岩、石英斑岩)分别进行了LA-ICP-MS锆石U-Pb同位素定年,获得加权平均年龄为(329.5±4.3)Ma、(324.6±4.6)Ma和(320.0±4.0)Ma,成岩时代为晚石炭世。地球化学表明,花岗岩具有富硅、略富铝,富钠低钾特征,属于钙碱性-高钾钙碱性、过铝质系列,具有I型花岗岩特征。稀土元素配分曲线为平缓型,轻重稀土元素分馏明显,负Eu 异常,微量元素富集Rb、Th和K,亏损Nb、Sr、P。综上所述,岩体形成于哈萨克斯坦-准噶尔板块与塔里木板块碰撞造山环境,成岩时代(329~320 Ma)早于成矿时代(272 Ma);相应成矿作用与康古尔韧性变形带的变形过程相耦合,具有韧性剪切带型金矿的特点。
英文摘要:
      In order to explore the coupling relationship between magmatism and mineralization of the Xifengshan gold deposit,LA-ICP-MS zircon U-Pb isotopic dating has been carried out for the ore bearing granitic rocks (veins) (granite, granite porphyry and quartz porphyry) in this paper, gives respectively a weighted average age of 329.5±4.3Ma、324.6±4.6Ma和 320.0±4.0Ma, indicating that the granites intruded in the Late Carboniferous Epoch . Geochemically, the granites are characterized by high contents of Si,Al, Na and low K,belong to series of high-K-calc-alkaline and peraluminous,which belonges to I type granite.Their REE and trace elements are enriched in LREE,Rb,Th and K, and differently depleted in Sr,Nb,P and Ti,with strong negative anomalies of Eu. The study shows that the granites (veins) formed in the compressional tectonic setting of the collisional orogeny between the Kazakhstan Junggar plate and the Tarim plat;The diagenetic age (329-320Ma) is obviously early the metallogenic age (272Ma), and is coupled with the deformation process of the Kangur ductile deformation zone.Therefore, it is considered that the deposit has the characteristics of ductile shear zone type gold deposits.
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