| 川西甲基卡花岗岩和新三号矿脉的形成时代及意义 |
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| 引用本文： | 郝雪峰,付小方,梁斌,袁蔺平,潘蒙,唐屹.川西甲基卡花岗岩和新三号矿脉的形成时代及意义[J].矿床地质,2015,34(6):1199-1208. |
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| 作者姓名： | 郝雪峰 付小方 梁斌 袁蔺平 潘蒙 唐屹 |
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| 作者单位： | 四川省地质调查院, 四川 成都 610081,四川省地质调查院, 四川 成都 610081,西南科技大学, 四川 绵阳 621010,四川省地质调查院, 四川 成都 610081,四川省地质调查院, 四川 成都 610081,西南科技大学, 四川 绵阳 621010 |
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| 基金项目： | 本文得到中国地质调查局"四川三稀资源综合研究与重点评价(编号:12120112208014)和"稀有稀土稀散矿产调查"项目的资助 |
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| 摘 要： | 锂被称为21世纪的能源金属,近年来在国内外受到了普遍重视。四川甲基卡矿田是中国乃至于世界上锂矿资源最集中的地区之一,近年来又发现了新三号矿脉。文章对矿田内唯一出露的马颈子花岗岩岩体中的锆石及岩体周围新三号花岗伟晶岩型锂矿脉中的锆石和铌钽矿物进行了LA-ICP-MS U-Pb同位素定年,分别获得(223±1)Ma、(216±2)Ma和(214±2)Ma的数据,表明成岩成矿作用发生于印支晚期,伟晶岩型稀有金属矿床的形成与马颈子岩体属于同期,因而含矿围岩原定为上三叠统新都桥组不合适,定为侏倭组更合理。
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| 关 键 词： | 地球化学 LA-ICP-MS U-Pb同位素定年 稀有金属 印支运动 伟晶岩型矿床 甲基卡 |
| 收稿时间： | 8/7/2015 12:00:00 AM |
| 修稿时间： | 2015/10/26 0:00:00 |
Formation ages of granite and X03 pegmatite vein in Jiajika,western Sichuan,and their geological significance |
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| HAO XueFeng,FU XiaoFang,LIANG Bin,YUAN LinPing,PAN Meng and TANG Yi.Formation ages of granite and X03 pegmatite vein in Jiajika,western Sichuan,and their geological significance[J].Mineral Deposits,2015,34(6):1199-1208. |
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| Authors: | HAO XueFeng FU XiaoFang LIANG Bin YUAN LinPing PAN Meng and TANG Yi |
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| Institution: | Geological Survey Institute of Sichuan Province, Chengdu 610081, Sichuan, China,Geological Survey Institute of Sichuan Province, Chengdu 610081, Sichuan, China,Southwest University of Science and Technology, Mianyang 621010, Sichuan, China,Geological Survey Institute of Sichuan Province, Chengdu 610081, Sichuan, China,Geological Survey Institute of Sichuan Province, Chengdu 610081, Sichuan, China and Southwest University of Science and Technology, Mianyang 621010, Sichuan, China |
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| Abstract: | Lithium is known as the 21st Century energy metal and hence attracts great inter est in recent years.With the recent discovery of X03 mega pegmatite Li mineral vein,the Jiajika orefield becomes one of the richest areas of Li resources in China and even in the world.In this study,the authors collected several zircon samples from the Majinzi granite and some niobium-tantalum mineral samples around the X03 vein in the Jiajika orefield,and conducted LA-ICP-MSU-Pb isotope dating of all these mineral samples.Three formation ages of(223±1) Ma,(216±2) Ma and(214±2) Ma were obtained.The results indicate that the pegmatite rare metal deposit has the same age with the granite,and the ore-forming and rock-forming process occurred in the Late Indosinian epoch.Therefore,the wall rocks of the pegmatite should be Zhuwo Formation rather than Xindujiao Formation. |
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| Keywords: | geochemistry LA-ICP-MS U-Pb isotope dating rare metal Indosinian Movement pegmatite deposit Jiajika |
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