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    粤北长江铀矿田辉长闪长岩的岩石成因及其与铀成矿的关系

    钟福军 潘家永 巫建华 夏菲 伏顺成 祁家明 赵奇峰

    钟福军, 潘家永, 巫建华, 夏菲, 伏顺成, 祁家明, 赵奇峰, 2019. 粤北长江铀矿田辉长闪长岩的岩石成因及其与铀成矿的关系. 地球科学, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592
    引用本文: 钟福军, 潘家永, 巫建华, 夏菲, 伏顺成, 祁家明, 赵奇峰, 2019. 粤北长江铀矿田辉长闪长岩的岩石成因及其与铀成矿的关系. 地球科学, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592
    Zhong Fujun, Pan Jiayong, Wu Jianhua, Xia Fei, Fu Shuncheng, Qi Jiaming, Zhao Qifeng, 2019. Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China. Earth Science, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592
    Citation: Zhong Fujun, Pan Jiayong, Wu Jianhua, Xia Fei, Fu Shuncheng, Qi Jiaming, Zhao Qifeng, 2019. Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China. Earth Science, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592

    粤北长江铀矿田辉长闪长岩的岩石成因及其与铀成矿的关系

    doi: 10.3799/dqkx.2017.592
    基金项目: 

    核资源与环境国家重点实验室自主基金项目 Z1608

    国家自然科学基金项目 U1403292

    江西省研究生创新项目 YC2016-B074

    中国地质调查局项目 12120115035601

    国家自然科学基金项目 41772066

    “十二五”国家科技支撑计划项目 2015BAB05B04

    详细信息
      作者简介:

      钟福军(1988-), 男, 讲师, 博士, 主要从事铀矿地质研究

      通讯作者:

      潘家永

    • 中图分类号: P612;P581

    Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China

    • 摘要: 长江铀矿田深部赋矿辉长闪长岩的岩石成因制约着对铀成矿作用认识的深入.通过对辉长闪长岩开展锆石U-Pb定年、Lu-Hf同位素、矿物学和地球化学分析,探讨其岩石成因、成岩构造背景及其与铀成矿的关系.辉长闪长岩LA-ICP-MS锆石U-Pb年龄为150 Ma,形成于晚侏罗世,具板内玄武岩地球化学特征.环带斜长石与黑云母主量元素变化记录了岩浆由基性到中性的演化过程.锆石(~150 Ma)εHft)为-14.1~-8.6,tDM2为1.7~2.1 Ga.辉长闪长岩源区为遭受俯冲带流体交代改造的相对富集地幔,岩浆上升侵位过程与中元古代-古元古代壳源物质发生了不同程度的地壳混染,形成于地壳伸展拉张和岩石圈大规模减薄的构造背景.辉长闪长岩为铀成矿提供了更为有利的还原性环境,促使热液中U6+的还原沉淀.

       

    • 图  1  长江铀矿田地质简图

      Hu et al.(2008)黄国龙等(2010).1.第四系; 2.燕山期中细粒二云母花岗岩; 3.燕山期中粒斑状黑云母花岗岩; 4.印支期粗粒二云母花岗岩; 5.印支期粗粒黑云母花岗岩; 6.加里东期花岗闪长岩; 7.中生代火山岩; 8.中生代花岗岩; 9.辉绿岩; 10.辉长闪长岩; 11.断裂构造带; 12.地质界线与推测地质界线; 13.铀矿床与名称; 14.乡镇

      Fig.  1.  Geological map of Changjiang uranium ore-field

      图  2  书楼坵矿床26号勘探线剖面示意图

      1.中粒黑云母花岗岩; 2.细粒黑云母花岗岩; 3.花岗斑岩; 4.辉长闪长岩; 5.碎裂蚀变带; 6.硅化破碎带; 7.铀矿体; 8.地质界线; 9.钻孔; 10.采样位置

      Fig.  2.  No.26 explorative section of Shulouqiu deposit

      图  3  辉长闪长岩与铀矿石野外与岩相学特征

      a.辉绿岩侵位于辉长闪长岩; b.辉长闪长岩手标本; c.辉长闪长岩单偏光图像; d.辉长闪长岩正交偏光图像; e.辉长闪长岩钻井岩芯; f.辉长闪长岩侵位于燕山期黑云母花岗岩; g.含铀矿化的辉长闪长岩; h.细脉状的沥青油矿; i.沥青油矿与黄铁矿. βμ.辉绿岩; δ.辉长闪长岩; Qtz.石英; Hb.角闪石; Py.黄铁矿; Mt.赤铁矿; Di.透辉石; Bt.黑云母; Kfs.钾长石; Fl.萤石; Ura.沥青铀矿; Chl.绿泥石

      Fig.  3.  Feld phenomenon and petrography of gabbro-diorite and uranium ore

      图  4  辉长闪长岩锆石U-Pb同位素年龄谐和图

      锆石CL图像中白色实线圈为U-Pb定年位置,括号外数据为206Pb/238U年龄,括号内为εHf(t)值

      Fig.  4.  Zircon U-Pb age concordia diagram of gabbro-diorite

      图  5  辉长闪长岩锆石εHf(t)直方图(a)与tDM2直方图(b)

      Fig.  5.  Histograms of zircon εHf (t)(a) and Hf isotopic model age(b)for gabbro-diorite

      图  6  环带斜长石剖面成分变化与正交偏光照片

      Fig.  6.  Section compositional variation and orthogonal polarization photo of zoned plagioclase

      图  7  斜长石An-Ab-Or三元分类图解

      Fig.  7.  The ternary classification diagram of An-Ab-Or for plagioclase

      图  8  黑云母剖面成分变化与BSE照片

      Fig.  8.  Section compositional variation and BSE photo of biotite

      图  9  黑云母成分分类

      Fig.  9.  Component classification of biotite

      图  10  单斜辉石分类图解

      Morimoto(1998).a.透辉石; b.次透辉石; c.普通辉石

      Fig.  10.  Classification diagram of clinopyroxene

      图  11  辉长闪长岩岩石类型(a)和岩石系列(b)判别图解

      图a据Winhchester and Floyd (1977);图b据Hastie et al. (2007)

      Fig.  11.  Classification diagrams of Zr/TiO2-Nb/Y (a) and Th-Co (b) for gabbro-diorite

      图  12  辉长闪长岩原始地幔标准化过渡元素蛛网图

      标准值据Taylor and McLennan (1985)

      Fig.  12.  Primitive mantle normalized transition element spider diagram for gabbro-diorite

      图  13  辉长闪长岩微量元素蛛网图(a)和稀土元素配分模式图(b)

      图a标准值据Sun and McDonough(1989);图b标准值据Taylor and McLennan (1985).粤北同期中基性岩据Li and McCulloch (1998);大陆拉斑玄武岩据Wilson (1989)

      Fig.  13.  Primitive mantle normalized trace element spider diagram (a) and chondrite normalized REE pattern (b) for gabbro-diorite

      图  14  黑云母MgO-(Fe2O3+FeO)/(Fe2O3+FeO+MgO)图解

      Fig.  14.  MgO-(Fe2O3+FeO)/(Fe2O3+FeO+MgO) diagram

      图  15  辉长闪长岩δEu-(La/Yb)N图解

      Fig.  15.  δEu-(La/Yb)N diagram of gabbro-diorite

      图  16  辉长闪长岩锆石Lu-Hf同位素组成

      Fig.  16.  Zircon Hf isotopic compsition of gabbro-diorite

      图  17  (Hf/Sm)N-(Ta/La)N (a)与Th/Zr-Nb/Zr (b)图解

      图a据la Flèche et al.(1998),图b据Kepezhinskas et al.(1997)

      Fig.  17.  (Hf/Sm)N-(Ta/La)N (a) and Th/Zr-Nb/Zr (b) diagrams

      图  18  辉长闪长岩La-La/Sm图解

      Fig.  18.  La vs. La/Sm diagram of gabbro-diorite

      图  19  辉长闪长岩成岩构造环境判别图解

      图a据Meschede (1986);图b据Pearce and Norry (1979);图c据Floyd and Winchester (1975);图d据Pearce (1983).WPA.板内碱性玄武岩; WPT.板内拉斑玄武岩; VAB.火山弧玄武岩

      Fig.  19.  Discriminated diagrams of tectonic setting for gabbro-diorite

      图  20  辉长闪长岩Th/Hf-Ta/Hf图解

      汪云亮等(2001)

      Fig.  20.  Th/Hf-Ta/Hf diagram for gabbro-diorite

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