[an error occurred while processing this directive] 世界地质 2020, 39(3) 509-527 DOI:   10.3969/j.issn.1004-5589.2020.03.002  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
LA-ICP-MS锆石U-Pb年龄
中基性脉岩
成矿时代
地球化学
宋家沟金矿
本文作者相关文章
何泽宇
申俊峰
王来明
李国武
刘汉栋
张华锋
杜佰松
吴晋超
PubMed
Article by He Z
Article by Shen J
Article by Wang L
Article by Li G
Article by Liu H
Article by Zhang H
Article by Du B
Article by Wu J
胶东宋家沟金矿中基性脉岩锆石U-Pb年代学、地球化学及其地质意义
何泽宇1, 申俊峰1, 王来明2, 李国武3, 刘汉栋2, 张华锋1, 杜佰松1, 吴晋超1
1. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
2. 山东省地质调查研究院, 济南 250013;
3. 中国地质大学(北京)科学研究院, 北京 100083
摘要: 胶莱盆地北缘宋家沟金矿分布众多与矿化相互交切的中基性脉岩,针对这些中基性脉岩开展了详细的LA-ICP-MS锆石U-Pb年代学、岩石学和地球化学研究。结果显示,中基性脉岩可以划分为成矿前和成矿后两类脉岩,岩石类型分别为辉绿岩和闪长岩,两者ΣREE含量均相对较高,成矿前脉岩LREE/HREE比值介于12.76~15.52,成矿后脉岩LREE/HREE比值为18.72,均表现出LREE相对富集,HREE相对亏损的特征。成矿前、后脉岩显著富集大离子亲石元素(Rb、Ba)和高场强元素(U、Th)等,亏损Nb、Ti等高场强元素,表现出受地壳物质混染的板内玄武岩特征。成矿前脉岩锆石U-Pb年龄介于518~802 Ma之间,属捕获锆石年龄,成矿后脉岩锆石U-Pb年龄为121±5 Ma,结合前人获得的莱阳群地层最大沉积年龄(130±2 Ma),认为宋家沟金矿床的形成时间为121~130 Ma。
关键词 LA-ICP-MS锆石U-Pb年龄   中基性脉岩   成矿时代   地球化学   宋家沟金矿  
LA-ICP-MS U-Pb dating, geochemistry and geological implications of intermediate-mafic dikes in Songjiagou gold deposit, eastern Shandong Province
HE Ze-yu1, SHEN Jun-feng1, WANG Lai-ming2, LI Guo-wu3, LIU Han-dong2, ZHANG Hua-feng1, DU Bai-song1, WU Jin-chao1
1. School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
2. Shandong Institute of Geological Survey, Jinan 250013, China;
3. Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China
Abstract: There are many intermediate-basic dikes which intersect the mineralization belts in Songjiagou gold deposit. Detailed zircon LA-ICP-MS U-Pb geochronology, petrology and geochemistry have been carried out for these intermediate-basic dikes.The results show that the dykes can be divided into pre-metallogenic and post-metallogenic dykes, which consist of diabase and diorite respectively.The ΣREE contents of the two types of dykes are relatively high, the LREE/HREE ratio of the pre-metallogenic dike ranges from 12.76 to 15.52,and the LREE/HREE ratio of the post-metallogenic dike is 18.72.Both are characterized by relative enrichment of LREE and depletion of HREE.The pre-metallogenic and post-metallogenic dikes are enriched in large ion lithophile elements(Rb, Ba) and high field-strength elements (U, Th), but depleted in Nb, Ti and other high field-strength elements, which show the characteristics of intraplate basalts mixed with crustal materials.The zircon U-Pb ages of the pre-metallogenic dikes range from 518 to 802 Ma, which belongs to the captured zircons, while the zircon U-Pb age of the post-metallogenic dyke is (121±5)Ma.Combined with the maximum sedimentary age of Laiyang Group (130±2 Ma),it is concluded that the Songjiagou gold deposit was formed in 121~130 Ma.
Keywords: zircon LA-ICP-MS U-Pb dating   intermediate-mafic dikes   metallogenic epoch   geochemistry   Songjiagou gold deposit  
收稿日期 2020-01-07 修回日期 2020-07-14 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2020.03.002
基金项目:

山东省地质勘查项目(鲁勘字[2018]19号)与国家重点研发计划“深地资源勘查开采”重点专项(2016YFC0600107)资助。

通讯作者: 申俊峰(1962-),男,博士,教授,主要从事矿物学教学与研究工作。E-mail:shenjf@cugb.edu.cn
作者简介:
作者Email: shenjf@cugb.edu.cn

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