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    辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄

    肖昌浩 刘向冲 赵岩 张青 陈正乐 刘建民 韦昌山 姚晓峰 王伟 解丽强

    肖昌浩, 刘向冲, 赵岩, 张青, 陈正乐, 刘建民, 韦昌山, 姚晓峰, 王伟, 解丽强, 2020. 辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄. 地球科学, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217
    引用本文: 肖昌浩, 刘向冲, 赵岩, 张青, 陈正乐, 刘建民, 韦昌山, 姚晓峰, 王伟, 解丽强, 2020. 辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄. 地球科学, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217
    Xiao Changhao, Liu Xiangchong, Zhao Yan, Zhang Qing, Chen Zhengle, Liu Jianmin, Wei Changshan, Yao Xiaofeng, Wang Wei, Xie Liqiang, 2020. Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China. Earth Science, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217
    Citation: Xiao Changhao, Liu Xiangchong, Zhao Yan, Zhang Qing, Chen Zhengle, Liu Jianmin, Wei Changshan, Yao Xiaofeng, Wang Wei, Xie Liqiang, 2020. Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China. Earth Science, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217

    辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄

    doi: 10.3799/dqkx.2020.217
    基金项目: 

    国家重点研发计划项目 2018YFC0603802

    国家自然科学基金项目 41702095

    中国地质调查局项目 DD20190161

    中国地质科学院基本科研业务费 JYYWF20180602

    详细信息
      作者简介:

      肖昌浩(1986-), 男, 助理研究员, 博士, 主要从事矿田构造和矿床学研究.ORCID:0000-0002-9815-6198.E-mail:xiaochanghao1986@126.com

    • 中图分类号: P618

    Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China

    • 摘要: 五龙金矿床是辽东地区最大的石英脉型金矿床,矿区内矿体和岩脉受断裂构造控制明显.容矿构造几何学和运动学特征显示,早白垩世初近NS向挤压形成的近NS向张裂隙、共轭的剪裂隙及派生一对共轭剪裂隙奠定五龙金矿床的构造格架.早白垩世的伸展导致闪长岩脉、三股流岩体、五龙背岩体等沿着先存构造薄弱带内充填,出溶的岩浆热液流体沿着闪长岩充填残余空间继续充填形成石英脉.由于右形剪切变形导致石英脉发生碎裂,并伴随着区域伸展,赋存闪长岩脉和石英脉的构造空间复活,随后花岗岩脉等侵位及出溶的成矿流体通过闪长岩脉上侵的通道运移和充填于石英脉裂隙中并交代闪长岩脉和片麻状二长花岗岩,最后造就了岩脉-矿化-蚀变同构造空间共存的现象.通过成矿期运动学特征显示,NE向断裂带与胶东三山岛金矿带矿体群侧伏规律相似,断裂带北段深部具有找矿潜力.五龙矿区而言,NE向断裂的找矿潜力优于NW向断裂带,NE向断裂下盘平行断裂内张性空间是盲矿体的有利空间.本次首次获得了五龙金矿床辉钼矿-黄铁矿-磁黄铁矿-石英阶段辉钼矿Re-Os同位素模式年龄为125±2.1 Ma.辉钼矿中Re含量为12.8×10-6,显示成矿物质具有壳幔混合的特征.对比前人研究,钼矿化和金成矿均与早白垩世构造体制转换下中国东部强烈的壳幔岩浆活动有关,为同一构造背景下的产物.通过对比胶东地区的成矿系列,辽东地区与胶东地区具有极大的相似性,存在两期钼矿化作用,尤其早白垩世晚期钼矿化可以作为寻找金矿的标志之一.

       

    • 图  1  辽东金矿区地质简图及主要金矿和钼铜矿分布

      Zhang et al.(2019)修编

      Fig.  1.  Geological map of the Liaodong Peninsula, showing the distribution of basements, Mesozoic igneous rocks and major gold deposits and molybdenum-copper deposits

      图  2  五龙矿集区地质图与剖面图

      a.据Feng et al.(2019)修编;b.据肖世椰等(2018)修编

      Fig.  2.  Geological maps of the Wulong gold district and a cross-section

      图  3  五龙金矿床含金石英脉与片麻状二长花岗岩面理方向斜交

      Fig.  3.  Auriferous quartz veins cross-cut the gneissic monzonitic granite in the Wolong deposit

      图  4  五龙金矿床含矿石英脉与岩浆岩平面图

      Zhang et al.(2019)修编

      Fig.  4.  Geological map of the Wulong gold deposit, showing major dike rocks, auriferous quartz veins and faults

      图  5  五龙金矿床辉钼矿-磁黄铁矿充填和交代自形-半自形黄铁矿

      Fig.  5.  Molybdenite intergrown with pyrrhotite and infilled in the pyrite or replaced the euhedral to subhedral pyrite

      图  6  五龙矿床蚀变特征

      Fig.  6.  Alteration characteristics in the Wulong deposit

      图  7  走滑断裂应力状态(a)、南北向挤压应力作用下可能的断裂组合(b)和走形力偶作用下可能的构造组合(c)

      σ1.最大主应力;σ3.最小主应力;R.里德尔剪切;R’.方向里德尔剪切;P.与R剪切对称的P剪切破裂;I.第一序次构造;II.第二序次构造

      Fig.  7.  Strike-slip faults at or near the surface of the earth (a), fault pattern under the N-S compression (b) and a fault system marked by straight runs, jogs that restrain, and jogs that release (open) (c)

      图  8  五龙金矿床22中段NW向163号矿体容矿构造变形特征

      Fig.  8.  Deformation characteristics of ore-bearing structures of No.163 orebody in the at -796 m in the Wulong gold deposit

      图  9  五龙金矿床19中段NNE向80号矿体容矿构造变形特征

      Fig.  9.  Deformation characteristics of ore-bearing structures of No. 80 orebody in the at -638 m in the Wulong gold deposit

      图  10  五龙金矿床48 m标高(二中段)矿脉分布(a)和五龙金矿床矿体横向投影(b)

      a.辽宁省有色地质局一〇三队内部资料修编;b.据肖国洪等(2003)

      Fig.  10.  Planar map showing orebodies at 48 m (a) and the projection map of the major orebody in the Wulong gold deposit (b)

      图  11  三山岛金矿带矿体垂直纵投影剖面

      张军进等(2016)

      Fig.  11.  The vertical projection of the major orebody in the Sanshandao ore belt

      图  12  辽东五龙矿集区成岩成矿年龄频谱图

      Fig.  12.  Geochronology framework of the Wulong gold district and associated magmatism in the Liaodong Peninsula, NE China

      表  1  五龙金矿床辉钼矿Re-Os同位素测试结果

      Table  1.   Re-Os isotopic analyses of molybdenite separating from the Wulong gold deposit

      样号 样重(g) Re(ng/g) 普Os(ng/g) 187Re(ng/g) 187Os(ng/g) 模式年龄(Ma)
      WL19-2 0.031 41 12 766 ±146 0.027 8 ±0.023 9 8 023 ±92 16.7 ±0.1 125 ±2.1
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