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    赣南黄沙铀矿区辉绿岩成因及其与铀成矿关系

    张熠阳 钟福军 潘家永 夏菲 祁家明 李海东 刘文泉

    张熠阳, 钟福军, 潘家永, 夏菲, 祁家明, 李海东, 刘文泉, 2022. 赣南黄沙铀矿区辉绿岩成因及其与铀成矿关系. 地球科学, 47(1): 206-223. doi: 10.3799/dqkx.2021.132
    引用本文: 张熠阳, 钟福军, 潘家永, 夏菲, 祁家明, 李海东, 刘文泉, 2022. 赣南黄沙铀矿区辉绿岩成因及其与铀成矿关系. 地球科学, 47(1): 206-223. doi: 10.3799/dqkx.2021.132
    Zhang Yiyang, Zhong Fujun, Pan Jiayong, Xia Fei, Qi Jiaming, Li Haidong, Liu Wenquan, 2022. Petrogenesis and Its Relationship with Uranium Mineralization of Diabase in Huangsha Uranium Ore-Field, South Jiangxi Province. Earth Science, 47(1): 206-223. doi: 10.3799/dqkx.2021.132
    Citation: Zhang Yiyang, Zhong Fujun, Pan Jiayong, Xia Fei, Qi Jiaming, Li Haidong, Liu Wenquan, 2022. Petrogenesis and Its Relationship with Uranium Mineralization of Diabase in Huangsha Uranium Ore-Field, South Jiangxi Province. Earth Science, 47(1): 206-223. doi: 10.3799/dqkx.2021.132

    赣南黄沙铀矿区辉绿岩成因及其与铀成矿关系

    doi: 10.3799/dqkx.2021.132
    基金项目: 

    国家自然科学基金项目 42002095

    国家自然科学基金项目 41772066

    国家自然科学基金项目 41862010

    核资源与环境国家重点实验室自主基金项目 Z1906

    核资源与环境国家重点实验室自主基金项目 2020Z08

    详细信息
      作者简介:

      张熠阳(1998-), 男, 硕士研究生, 研究方向为铀矿地质. ORCID: 0000-0001-9326-9014. E-mail: zyy292917338@163.com

      通讯作者:

      潘家永, ORCID: 0000-0002-6173-6009. E-mail: jypan@ecit.cn

    • 中图分类号: P612;P581

    Petrogenesis and Its Relationship with Uranium Mineralization of Diabase in Huangsha Uranium Ore-Field, South Jiangxi Province

    • 摘要:

      赣南黄沙铀矿区内发育的辉绿岩脉与铀矿化有着密切的空间关系,但其岩石成因研究薄弱,影响了对铀成矿过程的认识. 对辉绿岩进行了岩相学、主量元素、微量元素与Sr-Nd-Pb同位素分析. 结果显示,辉绿岩具有贫硅、贫碱、贫镁、Na2O > K2O、较富集大离子亲石元素、轻重稀土分馏不明显(LREE/HREE=2.81~2.97)、弱Eu异常(δEu=0.95~0.98)、典型Dupal异常铅、高(87Sr/86Sr)i(0.704 93~0.706 58)、低εNdt)(3.98~4.84)的地球化学特征,表明其属于大陆拉斑玄武岩系列,是在太平洋板块俯冲作用引起的岩石圈伸展减薄构造背景下,由软流圈物质与俯冲板片脱水产生的流体交代形成的岩石圈富集地幔相互作用后发生部分熔融形成的,岩浆在上升过程中经历了一定程度的结晶分异作用并与上地壳发生了混染. 综合研究认为矿区辉绿岩成岩作用(140 Ma)与铀成矿作用(100 Ma、63~76 Ma)存在巨大时差,辉绿岩为矿质沉淀提供了有利的赋矿空间和还原性环境. 通过与邻区诸广-下庄矿集区内辉绿岩对比,发现它们在成因上有相似性,与下庄矿田具有相似的控矿规律. 黄沙矿区成矿地质条件较优越,找矿潜力较好,下一步的找矿勘查应重点关注交点型铀矿化,重视NWW向辉绿岩脉与NE向破碎带交汇部位控矿.

       

    • 图  1  华南大地构造简图(改自Hu et al.,2008

      Fig.  1.  Geotectonic diagram of South China (modified from Hu et al., 2008)

      图  2  龙源坝岩体位置(a)和地质简图(b)

      a. 据Hu et al.,2008;b. 据钟福军等,2017

      Fig.  2.  Location (a) and geological sketch (b) of Longyuanba complex

      图  3  黄沙矿区地质简图

      据《南岭中段青嶂山矿集区铀矿找矿预测成果报告》,核工业二九〇研究所,2016

      Fig.  3.  Geological sketch of Huangsha ore-field

      图  4  上窖铀矿床16号带3号线(a)和15号带9号线剖面图(b)

      据《南岭中段青嶂山矿集区铀矿找矿预测成果报告》,核工业二九〇研究所,2016

      Fig.  4.  Section maps of prospecting line No.3 in the ore belt No.16 (a) and line No.9 in the ore belt No.15 (b) of Shangjiao uranium deposit

      图  5  黄沙矿区辉绿岩及铀矿石特征

      Amp.角闪石;Pl.斜长石;Mt.磁铁矿;Ptc.沥青铀矿;Hem.赤铁矿;Py.黄铁矿;Cal.方解石

      Fig.  5.  Pictures of diabase and uranium ore in Huangsha ore-field

      图  6  黄沙辉绿岩Zr/TiO2-Nb/Y图解(a)和Th-Co(b)图解

      图a据Winchester et al.1977),图b据Hastie et al.2007);诸广辉绿岩据田晓龙(2016);下庄辉绿岩据陆建军等(2006

      Fig.  6.  Zr/TiO2-Nb/Y (a) and Th-Co (b) diagrams of the Huangsha diabase

      图  7  黄沙辉绿岩微量元素蛛网图(a)和球粒陨石标准化稀土元素配分模式(b)

      MORB标准值据Pearce(1983);球粒陨石标准值据Taylor and McLennan(1985);诸广辉绿岩据田晓龙(2016);下庄辉绿岩据陆建军等(2006

      Fig.  7.  Trace element spider diagram (a) and chondrite-normalized rare earth element pattern (b) of the Huangsha diabase

      图  8  黄沙辉绿岩构造环境判别图解

      图a据Pearce and Cann(1973),其中A为岛弧拉斑玄武岩,B为MORB+岛弧拉斑玄武岩+钙碱性玄武岩,C为钙碱性玄武岩,D为板内玄武岩;图b据Pearce(1982);图c据Floyd et al.1975),其中A为碱性玄武岩,B为板内玄武岩,C为MORB;图d据Pearce et al.1979). 诸广辉绿岩据田晓龙(2016);下庄辉绿岩据陆建军等(2006

      Fig.  8.  Diagrams of discrimination for tectonic setting of the Huangsha diabase

      图  9  黄沙辉绿岩2Nb-Zr/4-Y(a)和Ta/Yb-Th/Yb(b)图解

      图a据Meschede(1986),其中WPA为板内碱性玄武岩,WPT为板内拉斑玄武岩,VAB为火山弧玄武岩;图b据Pearce(1983). 诸广辉绿岩据田晓龙(2016);下庄辉绿岩据陆建军等(2006

      Fig.  9.  2Nb-Zr/4-Y (a) and Ta/Yb-Th/Yb (b) diagrams of Huangsha diabase

      图  10  黄沙辉绿岩Pb-Pb(a)和Nd-Pb(b)图解

      DMMA、DMMB.亏损地幔端元;EMI、EMⅡ.富集地幔端元;HIMU.高U/Pb地幔端元;BSE.原始未分异地幔端元;PREMA.主流地幔端元;NHRL.北半球参考线(Zindler and Hart,1986);PPS.太平洋远洋沉积物(Chow and Patterson,1962);PFC.太平洋铁锰结壳(Ling et al.,1997);PT.太平洋浊积岩(Hemming and McLennan,2001);诸广辉绿岩据田晓龙(2016);下庄辉绿岩据陆建军等(2006

      Fig.  10.  Pb-Pb (a) and Nd-Pb (b) diagrams of the Huangsha diabase

      图  11  黄沙辉绿岩(La/Ta)N-(Th/Ta)N(a)、(La/Yb)N-δEu(b)、(Th/Ta)N-(La/Nb)N(c)和La/Ba-La/Nb(d)图解

      图c据Neal et al.2002);图d据Fitton et al.1991

      Fig.  11.  (La/Ta)N-(Th/Ta)N (a), (La/Yb)N-δEu (b), (Th/Ta)N-(La/Nb)N (c) and La/Ba-La/Nb (d) diagrams of Huangsha diabase

      图  12  黄沙辉绿岩Ba/La-Th/Yb(a)和Ba/Th-(La/Yb)N(b)图解

      Fig.  12.  Ba/La-Th/Yb (a) and Ba/Th-(La/Yb)N (b) diagrams of Huangsha diabase

      图  13  黄沙辉绿岩La-La/Sm图解

      Fig.  13.  La-La/Sm diagram of Huangsha diabase

      图  14  黄沙矿区交点型矿化示意图

      据《南岭中段青嶂山矿集区铀矿找矿预测成果报告》,核工业二九〇研究所,2016

      Fig.  14.  Schematic diagrams of intersection type mineralization in Huangsha ore-field

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