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高校地质学报 ›› 2024, Vol. 30 ›› Issue (01): 56-71.DOI: 10.16108/j.issn1006-7493.2022079

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贵东复式岩体中东部晚期花岗质小岩体的SHRIMP 锆石U-Pb 年龄及其地质意义

吴 佳1, 2,巫建华1, 2,刘晓东1, 2*,王凯兴1, 2,刘 帅1, 2   

  1. 1. 东华理工大学 地球科学学院,南昌 330013;
    2. 东华理工大学 核资源与环境国家重点实验室,南昌 330013
  • 出版日期:2024-02-18 发布日期:2024-02-18

Zircon SHRIMP U-Pb Ages and Geological Significance of the Late Stage Small Granitic Body in the Middle-Eastern Part of Guidong Complex Massif

WU Jia1,2,WU Jianhua1,2,LIU Xiaodong1,2*,Wang Kaixing1,2,LIU Shuai1,2   

  1. 1. School of Earth Science, East China University of Technology, Nanchang 330013, China;
    2. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
  • Online:2024-02-18 Published:2024-02-18

摘要: 贵东复式岩体由多期次、多类型的岩体组成,且东部盛产铀矿床,因此精确厘定该复式岩体的时代及其时序,查明复式岩体东部与中西部岩浆活动的差异性及其与铀成矿的关系,不仅有利于深入研究区域岩浆活动,而且有利于深刻认识铀的成矿规律。现有研究认为,以龟尾山断裂带为界,贵东复式岩体中西部岩基属燕山早期、东部岩基属印支早期,东部广泛发育的燕山期中基性脉岩与铀成矿关系密切。但对复式岩体中东部呈岩枝、岩株广泛出露的晚期花岗质小岩体的成岩地质时代及其分布规律尚存在争议,也有待进一步查明花岗质小岩体与铀矿床的时空关系。文章选择贵东复式岩体中东部晚期花岗质小岩体为研究对象,采用SHRIMP锆石U-Pb法厘定其成岩时代,并分析它们的时空分布及其与铀成矿的关系。测试结果显示,贵东复式岩体中东部晚期花岗质小岩体普遍存在高铀锆石,这可能是对同一岩体不同学者所获得的206Pb/238U加权平均年龄差别较大的主要原因。剔除高铀锆石的年龄数据,龟尾山断裂带以西的隘子、司前、陈洞岩体锆石206Pb/238U加权平均年龄分别为163.0±1.6 Ma、163.1±1.6 Ma、160.7±1.9 Ma,属燕山早期岩浆活动的产物;而以东的帽峰、分水坳、龟尾山岩体锆石206Pb/238U加权平均年龄分别为230.0±2.7 Ma、225.9±2.9 Ma和232.6±3.1 Ma,属印支期岩浆活动的产物。所以,龟尾山断裂以西和以东晚期花岗质小岩体的时代不同。且龟尾山断裂带以东的印支期花岗质小岩体空间上与铀矿化、尤其是与燕山早期的绢英岩化型等中高温热液铀矿化关系密切,是主要的储矿围岩;结合元素地球化学研究结果,该区产出的印支期花岗质小岩体也可为铀成矿提供铀源。

关键词: 贵东复式岩体, 花岗质小岩体, SHRIMP锆石U-Pb年龄, 铀成矿

Abstract: The Guidong complex massif composed of multistage and multi-type intrusive mass is the host rock for one of the most important granite-related uranium ore fields. However, up to now, the discovered uranium deposits are only distributed in the eastern part of this complex massif. In order to understand the relations of magmatism to uranium metallogenesis, it is crucial to understand the differences of petrological characteristics and to define the petrogenic ages of intrusive masses both in the eastern part and in middle-west part of Guidong complex massif. Taking the Guiweishan fault as the boundary roughly, the previous studies indicated that Guidong complex massif is dominated by early Yanshanian granitic batholith in the middle-western part and by early Indosinian granitic batholith with late stage mafic dykes in the eastern part. It is generally agreed that the late-stage mafic dykes of Yanshanian ages closely link to uranium mineralization. However, the ages of widely distributed late-stage small granitic bodies in the middle-eastern part of Guidong complex massif are still under debate, and further study is necessary to reveal the spatial-temporal relationship and the possible genetic links of late-stage small granitic bodies to uranium mineralization. Zircon SHRIMP U-Pb dating of the late-stage small granitic bodies in the middle-eastern part of Guidong complex massif was conducted in this paper. The results show that highuranium zircons are common in the late-stage small granitic bodies, which can explain the difference of zircon U-Pb ages from a granite body by different scholars. Eliminating the 206Pb/238U ages with high-uranium zircons in the weighted average age data processing, samples collected from the Aizi, Siqian and Chendong granitic bodies in the western part of the Guiweishan fault yielded the early Yanshanian magmatism with the 206Pb/238U zircon weighted average ages of 163.0±1.6

Ma, 163.1±1.6 Ma and 160.7±1.9 Ma, respectively. While samples collected from the Maofeng, Fenshuiao and Guiweishan granitic bodies in the eastern part of the Guiweishan fault yielded the Indosinian magmatism with the 206Pb/238U zircon weighted average ages of 230.0±2.7 Ma, 225.9±2.9 Ma and 232.6±3.1 Ma, respectively. Therefore, the ages of the late-stage small granitic bodies in the middle-eastern part of Guidong complex massif are diverse in different locations. As the host rock of uranium deposits, the Indosinian small granites in the eastern part of the Guiweishan fault have the close links to high temperature sericitization type uranium mineralization. And the small granitic bodies may also provide the uranium sources based on the results of previous element geochemical st udies. 

Key words: Guidong complex massif, small granitic body, zircon SHRIMP U-Pb age, uranium mineralization

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