DOI:
矿床地质:2014,Vol.>>Issue(2):397-405

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
中国地质科学院矿产资源研究所 国土资源部成矿作用和资源评价重点实验室, 北京 100037;中国地质科学院矿产资源研究所 国土资源部成矿作用和资源评价重点实验室, 北京 100037;中国地质科学院矿产资源研究所 国土资源部成矿作用和资源评价重点实验室, 北京 100037;中国地质科学院矿产资源研究所 国土资源部成矿作用和资源评价重点实验室, 北京 100037;金玛宽甸矿业有限公司, 辽宁 丹东 118200;北京科技大学土木与环境工程学院, 北京 100083
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
HU GuYue,FAN ChangFu,LI YanHe,HOU KeJun,LIU Yi,WANG TianHui
(MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Jinma Kuandian Mining Co., Ltd., Dandong 118200, Liaoning, China;Civil and Environment Engineering School, University of Science and Technology Beijing, Beijing 100083, China)
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投稿时间:2013-03-27   修订日期:2013-12-26      网络发布日期:2014-04-26
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。
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.
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中图分类号:P618.21+9;P618.46     
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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
引用文本:
胡古月,范昌福,李延河,侯可军,刘,王天慧.2014.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[J].矿床地质,33(2):397~405
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 Deposits33(2):397~405
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