| 辽东明安硼镁矿床混合花岗岩的锆石U-Pb年龄及对成矿时代的制约 |
| Received:March 27, 2013 Revised:December 26, 2013 点此下载全文 |
| 引用本文：HU GuYue,FAN ChangFu,LI YanHe,HOU KeJun,LIU Yi,WANG TianHui.2014.Zircon U-Pb dating of migmatitic granites of Ming’an Mg-borate deposit in Kuandian area, eastern Liaoning Province, and its constrains on mineralization age[J].Mineral Deposits,33(2):397~405 |
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| Author Name | Affiliation | E-mail | | HU GuYue | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | FAN ChangFu | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | fancf@cags.ac.cn | | LI YanHe | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | HOU KeJun | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | LIU Yi | Jinma Kuandian Mining Co., Ltd., Dandong 118200, Liaoning, China | | | WANG TianHui | Civil and Environment Engineering School, University of Science and Technology Beijing, Beijing 100083, China | |
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| 基金项目:本文得到国土资源部公益性行业科研专项经费项目（项目号：201211074-2）资助 |
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| 中文摘要:辽东硼矿赋存于辽吉裂谷中央凹陷带内的里尔峪组地层中，形成于火山活动与蒸发沉积交替旋回的环境，后期经历了低压角闪岩相至混合岩化变质作用，属沉积-变质型硼矿床，主矿区包括有后仙峪、翁泉沟和砖庙-杨木杆三处。混合岩化作用使裂谷早期喷发的酸性火山岩发生原地重熔，形成大量层状产出的混合花岗岩、变粒岩和浅粒岩。文章利用LA-MC-ICP-MS技术对砖庙-杨木杆矿区明安硼镁矿体下盘，与上部地层发生同构造变形的层状混合花岗岩进行了锆石U-Pb年龄的测定，尝试解决明安硼矿的成矿时代问题。混合花岗岩的锆石阴极发光图像显示，锆石具有核-边结构，核部的震荡环带为岩浆成因，边部为变质增生成因。锆石核部的U-Pb定年结果表明：207Pb/206Pb加权平均年龄为（2229±3）Ma（MSWD=0.8），Th/U值为0.4479~1.1309。因此，笔者认为（2229±3）Ma年龄代表了层状混合花岗岩原岩——酸性火山岩的喷发时代，也代表了硼镁矿的初始含硼蒸发岩形成时代的下限。 |
| 中文关键词:地球化学 LA-MC-ICP-MS锆石U-Pb年龄 混合花岗岩 明安硼镁矿床 辽河群 里尔峪组 |
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| Zircon U-Pb dating of migmatitic granites of Ming’an Mg-borate deposit in Kuandian area, eastern Liaoning Province, and its constrains on mineralization age |
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| Abstract:Borate deposits in eastern Liaoning belong to a metamorphic volcano-sedimentary mineral type, and are distributed in the central part of "Liao-Ji rift". They were formed in an environment of volcanism and evaporation, and commonly experienced amphibolite facies metamorphism and migmatitization. The main ore districts include Houxianyu, Wenquangou and Zhuangmiao-Yangmugan Mg and Mg-Fe borate ore districts. Due to the regional intense migmatitization, the acid volcanic rocks were melted in-situ, and large mounts of layered migmatitic granites, leptites and leptynites were formed. This paper reports an integrated study of U-Pb zircon age (LA-MC-ICP-MS) of the layered migmatitic granites in the Ming'an borate deposit of the Zhuangmiao-Yangmugan ore district. This study may give a solution of the timing of the volcanic-sedimentary association and borate deposits. The zircon CL images of the migmatitic granites show that they have uniform core-rim microstructures, the cores have preserved the magmatic zone, and the rims display metamorphic structure. The U-Pb analyses of the magmatic core show a weighted mean 207Pb/206Pb age of (2229±3) Ma (MSWD=0.8) and Th/U ratios of 0.4479~1.1309. It is thus held that the weighted mean age of (2229±3) Ma might represent the lower limit forming age of the boron-bearing evaporites. |
| keywords:geochemistry LA-MC-ICP-MS zircon U-Pb dating migmatitic granite Ming’an Mg-borate deposit Liaohe Group Lieryu Formation |
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