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现代地质 ›› 2016, Vol. 30 ›› Issue (1): 59-68.

• 岩石学 • 上一篇    下一篇

北武夷王坞矿区花斑岩与钼矿的关系：来自锆石U-Pb和辉钼矿Re-Os定年的证据

魏娟娟1,2，狄永军1，魏英文3，张达1，罗平3，罗国辉3，秦晓峰1，董越1，杨秋1，陈杰1   

  1. (1.中国地质大学(北京)地球科学与资源学院，北京 100083；2.上饶市广丰区国土资源局，江西 上饶 334600；
    3.江西省地质矿产勘查开发局 赣东北大队，江西 上饶 334000)
  • 出版日期:2016-01-29 发布日期:2016-05-01
  • 通讯作者: 狄永军，男，副教授，博士，1965年出生，岩石学、矿物学、矿床学专业，从事岩浆作用与成矿方面的研究。 Email：diyongjun@cugb.edu.cn
  • 作者简介:魏娟娟，女，硕士，1989年出生，地质工程专业，主要从事岩浆作用与成矿方面的研究及矿产资源开发管理方面的工作。Email：jjwei1989@163.com。
  • 基金资助:

    中国地质调查局项目(1212011220557)。

Relationship Between Granophyre and Molybdenum Ore of Wangwu Mining District in North Wuyi Region: Evidences from Zircon U-Pb and Molybdenite Re-Os Dating

gWEI Juan-juan1,2，DI Yong-jun1，WEI Ying-wen3，ZHANG Da1 ，LUO Ping3，LUO Guo-hui3，QIN Xiao-feng1，DONG Yue1，YANG Qiu1，CHEN Jie1   

  1. (1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. Bureau of Land and Resources of Guangfeng District, Shangrao, Jiangxi 334600, China;
    3. Northeastern Jiangxi Geological Party, Bureau of Geology and Mineral Resources of Jiangxi Province, Shangrao, Jiangxi 334000, China)
  • Online:2016-01-29 Published:2016-05-01

PDF (PC)

17041

摘要：

王坞钼铜矿床是北武夷地区近年来发现并正在勘查的具大型规模以上潜力的矿床。在矿床地质特征研究的基础上，通过锆石LA-ICP-MS U-Pb法测年，获得矿区中与钼矿体在空间上关系密切的花斑岩脉的加权平均年龄为(127.5±1.8) Ma(MSWD=1.4)，说明其形成于早白垩世；通过辉钼矿Re-Os法测年，获得辉钼矿Re-Os等时线年龄为(153.7±3.2) Ma(MSWD=3.9)，说明钼矿形成于晚侏罗世。因此，花斑岩脉的成岩时代远远晚于钼矿成矿时代，表明两者无成因联系。通过对比邻区矿床成矿特征并结合现有资料分析，推断王坞矿区成钼岩体为酸性花岗斑岩或黑云母花岗岩，位于南东方向深部，深部找矿前景较好。北武夷地区中生代主要成钼时期为晚侏罗世早期(155 Ma±)和早白垩世早期(135 Ma±)，该时期钼铜矿的形成与古太平洋板块俯冲形成的弧岩浆活动有关。

关键词: Re-Os定年, 锆石U-Pb定年, 辉钼矿, 花斑岩, 王坞, 北武夷

Abstract:

 The Wangwu Mo-Cu deposit is one that has been explorating and has the potential of large or super-large scale in recent years in North Wuyi region. Based on the study of geological feature, with LA-ICP-MS zircon U-Pb dating, the granophyre vein weighted mean age is (127.5±1.8) Ma(MSWD=1.4).It is shown that the deposit formed in Early Cretaceous Epoch. Using molybdenite Re-Os dating, the isochron age is (153.7±3.2) Ma(MSWD=3.9). It indicates that metallogenesis of Mo occurred in Late Jurassic Epoch. The diagenesis age of granophyre vein is much later than that of Mo deposit, which shows that there is no relationship between them. Comparing the neighbor deposit mineralization feature and analyzing the existed information, it infers that the rock of molybdenum is acidic granite porphyry or biotite granite, which is located in the deep area of southeastern part of the ore district. The major metallogenesis age of Mo is Early-Late Jurassic Epoch (155 Ma±) and Early Cretaceous Epoch(135 Ma±) in North Wuyi area. During this period, the formation of Mo and Cu deposits are related to magmation caused by paleopacific plate subducting.

Key words: Re-Os dating, zircon U-Pb dating, molybdenite, granophyre, Wangwu, North Wuyi region

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