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    兴蒙造山带的基底属性与构造演化过程

    许文良 孙晨阳 唐杰 栾金鹏 王枫

    许文良, 孙晨阳, 唐杰, 栾金鹏, 王枫, 2019. 兴蒙造山带的基底属性与构造演化过程. 地球科学, 44(5): 1620-1646. doi: 10.3799/dqkx.2019.036
    引用本文: 许文良, 孙晨阳, 唐杰, 栾金鹏, 王枫, 2019. 兴蒙造山带的基底属性与构造演化过程. 地球科学, 44(5): 1620-1646. doi: 10.3799/dqkx.2019.036
    Xu Wenliang, Sun Chenyang, Tang Jie, Luan Jinpeng, Wang Feng, 2019. Basement Nature and Tectonic Evolution of the Xing'an-Mongolian Orogenic Belt. Earth Science, 44(5): 1620-1646. doi: 10.3799/dqkx.2019.036
    Citation: Xu Wenliang, Sun Chenyang, Tang Jie, Luan Jinpeng, Wang Feng, 2019. Basement Nature and Tectonic Evolution of the Xing'an-Mongolian Orogenic Belt. Earth Science, 44(5): 1620-1646. doi: 10.3799/dqkx.2019.036

    兴蒙造山带的基底属性与构造演化过程

    doi: 10.3799/dqkx.2019.036
    基金项目: 

    国家自然科学基金项目 41772047

    国家自然科学基金项目 41702051

    国家自然科学基金项目 41330206

    详细信息
      作者简介:

      许文良(1959-), 男, 教授, 博士生导师, 主要从事火成岩石学研究

      通讯作者:

      许文良

    • 中图分类号: P581

    Basement Nature and Tectonic Evolution of the Xing'an-Mongolian Orogenic Belt

    • 摘要: 为了解兴蒙造山带基底属性和多个构造体系演化与叠加历史,系统总结了近年来在基础地质研究中取得的新成果,并利用这些成果讨论了兴蒙造山带的基底属性与演化历史.兴蒙造山带是指我国东北地区古生代构造作用影响的地区,这些地区也遭受了中生代构造作用的叠加与改造.兴蒙造山带主要由微陆块和其间的造山带组成.虽然传统上认为属于前寒武纪结晶基底的地质体主要已解体为古生代和早中生代,但随着新太古代和古元古代地质体的相继发现,以及新生代玄武岩中幔源古元古代橄榄岩包体的发现,可以判定兴蒙造山带内微陆块应具有古老的前寒武纪基底,并且壳幔是耦合的.微陆块内部地壳增生以垂向增生为主,且主要发生在新元古代和中元古代,以及次要的新太古代和古生代.相反,陆块间造山带或岛弧地体的陆壳则以侧向增生为主,且主要发生在新元古代和古生代.额尔古纳地块与兴安地块的拼合发生在早古生代早期;兴安地块与松嫩地块的拼合发生在早石炭世晚期;松嫩地块与佳木斯地块的拼合发生在早古生代晚期,中生代早期又经历了裂解与再闭合的构造演化过程;华北克拉通北缘增生杂岩带与北方微陆块群的最终拼合发生在晚二叠世-中三叠世,古亚洲洋的最终闭合发生在中三叠世,且为剪刀式闭合.晚古生代晚期蒙古-鄂霍茨克大洋板块南向俯冲作用的发生以及早中生代(三叠纪-早侏罗世)的持续南向俯冲,控制了大兴安岭-冀北-辽西地区的岩浆活动,蒙古-鄂霍茨克大洋的闭合发生在中侏罗世,晚侏罗世-早白垩世主要表现为闭合后的伸展环境.古太平洋板块中生代的俯冲起始时间为早侏罗世,晚侏罗世-早白垩世早期东北亚陆缘主要表现为走滑的构造属性和陆缘地体从低纬度到高纬度的构造就位过程,早白垩世晚期-古近纪岩浆作用的向东收缩揭示了古太平洋板块的持续俯冲和俯冲板片的后撤过程,古近纪晚期日本海的打开标志着东北亚陆缘从活动陆缘已经转变为沟-弧-盆体系,并且标志着东亚大地幔楔的形成.

       

    • 图  1  兴蒙造山带构造单元划分

      Wu et al.(2007b)

      Fig.  1.  Simplified geological map of main tectonic subdivisions in the Xing′an-Mongolian Orogenic Belt

      图  2  兴蒙造山带微陆块中前寒武纪地质体分布

      Fig.  2.  Distribution map of Precambrian terranes within microcontinental massifs in the Xing′an-Mongolian Orogenic Belt

      图  3  额尔古纳地块中花岗质岩浆作用的期次

      Fig.  3.  Probability plot of granitoid magmatic event ages within the Erguna massif

      图  4  额尔古纳地块花岗岩锆石Hf同位素二阶段模式年龄频谱与地壳增生

      Fig.  4.  Probability plot of zircon TDM2(Hf) ages from granitoids and crustal accretion within the Erguna massif

      图  5  额尔古纳地块花岗岩年龄与锆石Hf同位素二阶段模式年龄变异图

      Fig.  5.  Plot of zircon TDM2(Hf) ages against granitoid ages within the Erguna massif

      图  6  多宝山岛弧地体古生代-中生代花岗岩年龄与锆石Hf同位素组成变异图

      Fig.  6.  Plots of zircon Hf compositions (TDM2(Hf) ages and εHf values) against the ages of Paleozoic-Mesozoic granitoids from Duobaoshan island arc terrane

      图  7  额尔古纳地块、兴安地块和松嫩地块间的缝合线位置

      Li et al., 2017b;①德尔布干断裂;②喜桂图-塔源缝合带;③黑河-嫩江-贺根山断裂;④黑河-嫩江缝合带

      Fig.  7.  Locations of the suture zones between the Erguna and Xing′an massifs as well as the Xing′an and Songnen massifs

      图  8  牡丹江洋的形成与黑龙江杂岩构造就位模式

      孙晨阳等(2018);SNM.松嫩地块;JM.佳木斯地块

      Fig.  8.  A model for the formation of the Mudanjiang Ocean and tectonic emplacement of the Heilongjiang complex

      图  9  兴凯地块、松嫩地块和佳木斯地块构造关系

      Xu et al.(2018)

      Fig.  9.  Tectonic relation map for the Khanka, Songnen and Jiamusi massifs

      图  10  华北克拉通北缘早中生代地层物源变化与古亚洲洋最终闭合过程

      Wang et al.(2018)

      Fig.  10.  Provenance variation of the Early Mesozoic strata in the northern margin of the North China craton and the final closure process of the Paleo-Asian Ocean

      图  11  蒙古-鄂霍茨克构造体制与环太平洋构造体制早侏罗世-新生代演化模式

      Tang et al.(2018)修改;SC.西伯利亚克拉通;XMOB.兴蒙造山带;SAOB.锡霍特-阿林造山带

      Fig.  11.  The evolutionary model for the Mongol-Okhotsk and circum-Pacific tectonic regimes during the Early Jurassic-Cenozoic

      图  12  中国东北及俄罗斯滨海边疆区白垩纪-古近纪岩浆活动时空变异

      孙明道(2016)

      Fig.  12.  Spatial-temporal variations of the Cretaceous-Paleocene magmatisms in NE China and Russian Far East

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    • 收稿日期:  2019-01-02
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