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    华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统

    赵新福 李占轲 赵少瑞 毕诗健 李建威

    赵新福, 李占轲, 赵少瑞, 毕诗健, 李建威, 2019. 华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统. 地球科学, 44(1): 52-68. doi: 10.3799/dqkx.2018.372
    引用本文: 赵新福, 李占轲, 赵少瑞, 毕诗健, 李建威, 2019. 华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统. 地球科学, 44(1): 52-68. doi: 10.3799/dqkx.2018.372
    Zhao Xinfu, Li Zhanke, Zhao Shaorui, Bi Shijian, Li Jianwei, 2019. Early Cretaceous Regional-Scale Magmatic-Hydrothermal Metallogenic System at the Southern Margin of the North China Carton. Earth Science, 44(1): 52-68. doi: 10.3799/dqkx.2018.372
    Citation: Zhao Xinfu, Li Zhanke, Zhao Shaorui, Bi Shijian, Li Jianwei, 2019. Early Cretaceous Regional-Scale Magmatic-Hydrothermal Metallogenic System at the Southern Margin of the North China Carton. Earth Science, 44(1): 52-68. doi: 10.3799/dqkx.2018.372

    华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统

    doi: 10.3799/dqkx.2018.372
    基金项目: 

    中央高校基本科研业务费专项资金 CUGCJ1711

    国家自然科学基金项目 41772074

    国家自然科学基金项目 91514303

    国家自然科学基金项目 41822203

    中央高校基本科研业务费专项资金 CUG140618

    详细信息
      作者简介:

      赵新福(1982-), 男, 教授, 主要从事矿床学教学和研究工作

      通讯作者:

      赵新福

      李占轲

    • 中图分类号: P611

    Early Cretaceous Regional-Scale Magmatic-Hydrothermal Metallogenic System at the Southern Margin of the North China Carton

    • 摘要: 华北克拉通南缘在中生代发生了大规模的成矿作用,主要的矿床类型有脉状金矿床(石英脉型、构造蚀变岩型)、斑岩型钼矿床、脉状银铅锌矿床.对于这些矿床的成因和成矿动力学背景,目前还存在不少争议.但近年来越来越多的成矿年代学证据表明,这些矿床均主要形成于早白垩世,且与区域上广泛发育的岩浆活动具有高度的时空一致性.在归纳总结华北克拉通南缘主要矿床类型地质特征和时空分布的基础上,简述各类矿床的成矿物质来源以及它们之间的成因联系,指出这些不同类型的矿床组成了一个巨型的岩浆-热液成矿系统.华北克拉通南缘成矿作用与其邻近的东秦岭-大别成矿带的成矿作用具有一致性,均受中国东部早白垩世大规模伸展作用控制,是统一的地球动力学背景下的产物.结合地球物理的资料认为,早白垩世岩石圈伸展及其导致的岩浆作用最可能与晚中生代古太平洋板块向东亚大陆边缘俯冲作用有关.上涌的岩浆热液在合适的构造体制下,与上地壳的岩石和流体发生交代和流体混合,最终在浅部形成大规模的岩浆-热液成矿系统.

       

    • 图  1  华北克拉通中生代主要矿床类型及其分布

      Zhao et al.(2012a)修改

      Fig.  1.  The distribution of major Mesozoic deposits in North China Craton

      图  2  华北克拉通南缘地质简图及主要类型的矿床分布

      修改自Mao et al.(2010)

      Fig.  2.  Simplified geological map of the south margin of the North China Craton, also showing the locations of major deposit types

      图  3  红土岭矿床钼(a~c)、金(d~f)矿脉石英中流体包裹体对比

      Fig.  3.  Comparison of fluid inclusions from the Mo (a-c) and Au (d-f) veins from the Hongtuling deposit

      图  4  华北克拉通南缘大湖、红土岭金-钼矿脉及小秦岭碳酸岩型钼矿Pb同位素组成对比

      大湖和红土岭数据来自笔者未发表数据;碳酸岩型钼矿包括黄龙埔和黄水庵,数据黄典豪等(1984, 2009)

      Fig.  4.  Comparison of Pb isotopes for the Dahu and Hongtuling lode Au-Mo deposits and the carbonatite related Mo deposits from the southern margin of the North China Craton

      图  5  南泥湖矿田斑岩型-矽卡岩型钼(钨)矿-矽卡岩型硫铁铅锌矿-热液脉型银铅锌矿成矿系列示意

      图改自李占轲(2013);年龄数据李永峰等(2005)叶会寿等(2006)向君峰等(2012)李占轲(2013)杨晨英等(2016)

      Fig.  5.  A sketch showing a metallogenic system for the porphyry-skarn Mo-(W), skarn Pb-Zn, and lode Pb-Zn-Ag deposits in the Nannihu orefield

      图  6  华北克拉通南缘侏罗纪-白垩纪岩浆岩及典型类型矿床年龄统计结果

      数据主要引自Li et al.(2012a)李占轲(2013)唐克菲(2014)

      Fig.  6.  Histogram for the Jurassic-Cretaceous intrusions and major deposit types for the southern margin of North China Craton

      图  7  华北克拉通南缘晚中生代金矿床、钼矿床和银铅锌矿床Pb同位素组成对比

      铅同位素数据主要来源:小秦岭金矿床据聂凤军等(2001)赵海香(2011);熊耳山金矿床据王炯辉等(2016)张苏坤等(2016);斑岩型钼矿床据焦建刚等(2010)李洪英等(2011)Li et al.(2017);银铅锌矿床据陈衍景等(2003)Li et al.(2013, 2016)

      Fig.  7.  Pb isotope for Au, Mo, and Pb-Zn-Ag deposits at the southern margin of the North China Craton

      图  8  华北克拉通南缘早白垩世成矿模式示意图及不同矿床类型间的成因联系

      修改自李占轲(2013)

      Fig.  8.  A sketch showing the possible genetic links between the Early Cretaceous deposit types in the southern margin of the North China Craton

      图  9  华北克拉通南缘及东秦岭-桐柏-大别岩浆岩分布及早白垩世斑岩钼矿床、脉状金矿床和银铅锌矿床分布图

      底图据高昕宇等(2017)

      Fig.  9.  A simplified map showing the Early Cretaceous intrusions and porphyry Cu, lode Au and Au-Pb-Zn deposits in both southern margin of the North China Craton and eastern Qinling-Dabie orogen

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