中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约

许文良, 王枫, 裴福萍, 孟恩, 唐杰, 徐美君, 王伟. 2013. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约. 岩石学报, 29(2): 339-353.
引用本文: 许文良, 王枫, 裴福萍, 孟恩, 唐杰, 徐美君, 王伟. 2013. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约. 岩石学报, 29(2): 339-353.
XU WenLiang, WANG Feng, PEI FuPing, MENG En, TANG Jie, XU MeiJun, WANG Wei. 2013. Mesozoic tectonic regimes and regional ore-forming background in NE China: Constraints from spatial and temporal variations of Mesozoic volcanic rock associations. Acta Petrologica Sinica, 29(2): 339-353.
Citation: XU WenLiang, WANG Feng, PEI FuPing, MENG En, TANG Jie, XU MeiJun, WANG Wei. 2013. Mesozoic tectonic regimes and regional ore-forming background in NE China: Constraints from spatial and temporal variations of Mesozoic volcanic rock associations. Acta Petrologica Sinica, 29(2): 339-353.

中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约

  • 基金项目:

    本文受国家重点基础研究发展计划资助(2013CB429803);国家自然科学基金项目(41272077、90814003)和中国地质调查局项目(1212011085480、1212011085476)联合资助.

详细信息
    作者简介:

    许文良,男,1959年生,博士,教授,主要从事火成岩成因与岩石圈动力学研究,E-mail: xuwl@jlu.edu.cn

  • 中图分类号: P588.14;P597.3

Mesozoic tectonic regimes and regional ore-forming background in NE China: Constraints from spatial and temporal variations of Mesozoic volcanic rock associations

  • 本文系统总结了东北地区中生代火山岩的年代学、岩石组合及其时空分布规律,以便对环太平洋构造体系和蒙古-鄂霍茨克构造体系中生代的演化历史及其东北地区中生代区域成矿背景给出制约。基于火山岩中锆石U-Pb定年结果,东北地区中生代火山作用可划分成六期:晚三叠世(200~228Ma)、早-中侏罗世(173~190Ma)、中-晚侏罗世(158~166Ma)、早白垩世早期(138~145Ma)、早白垩世晚期(106~133Ma)和晚白垩世(88~97Ma)。晚三叠世火山作用主要分布在吉黑东部和小兴安岭-张广才岭地区,前者为A型流纹岩,后者为双峰式火山岩组合,它们共同揭示了古亚洲洋最终闭合后的伸展环境;早-中侏罗世火山岩主要分布在吉黑东部、小兴安岭-张广才岭和额尔古纳地区,吉黑东部和额尔古纳地区早-中侏罗世钙碱性火山岩的存在分别标志着古太平洋板块和蒙古-鄂霍茨克洋板块俯冲作用的发生,而小兴安岭-张广才岭早-中侏罗世火山岩则以双峰式火成岩组合为特征,反映了双向俯冲的弧后伸展环境;中-晚侏罗世和早白垩世早期火山岩主要分布在松辽盆地以西和冀北-辽西地区,前者为碱性-亚碱性的过渡系列,主要由玄武粗安岩、粗安岩和少量粗面岩组成,后者为A型流纹岩或碱性流纹岩组成,这些火山岩形成于加厚陆壳的坍塌或拆沉阶段;早白垩世晚期火山岩广泛分布于东北地区,吉黑东部为钙碱性火山岩组合,而松辽盆地和大兴安岭地区则主要为双峰式火山岩组合,前者标志着古太平洋板块的俯冲,后者与早期加厚陆壳的拆沉和/或类似弧后的伸展环境有关;晚白垩世火山岩主要分布在吉黑东部和陆内,前者为钙碱性火山岩组合,后者为碱性玄武岩,反映了来自东部环太平洋构造体系的俯冲作用。综合上述中生代火山岩的岩石组合及时空分布特征,可以判定:1)环太平洋构造体系对东亚大陆下的俯冲始于早侏罗世,中生代期间存在早侏罗世、早白垩世晚期和晚白垩世三次俯冲事件,其影响的空间范围主要在松辽盆地及其以东地区,陆缘和古俯冲带是寻找斑岩型矿床的有利场所,而陆内的伸展区域主要与浅成低温热液矿床有关;2)蒙古-鄂霍茨克构造体系经历了中生代早期的俯冲事件和中侏罗世及早白垩世早期两次陆内推覆事件,其影响的空间范围主要在松辽盆地以西地区和华北地块北缘,中生代早期的俯冲事件主要与活动陆缘背景下的斑岩型矿床关系密切,而晚侏罗世和早白垩世两次与加厚陆壳拆沉有关的伸展背景有利于多金属矿床的形成。

  • 加载中
  • 图 1 

    东北地区的构造分区(a, 据Wu et al., 2011)和东北的主要地理单元(b, 据Meng, 2003)

    Figure 1. 

    Tectonic subdivisions of northeastern (NE) China (a, after Wu et al., 2011) and main topographical units in NE China (b, afterMeng, 2003)

    图 2 

    中国东北中生代火山岩锆石U-Pb年龄频数图

    Figure 2. 

    Probability plots of the zircon U-Pb ages for the Mesozoic volcanic rocks in NE China

    图 3 

    东北地区中生代火山岩的分布图

    Figure 3. 

    Distribution map of Mesozoic volcanic rocks in NE China

    图 4 

    东北地区早中生代斑岩型矿床分布图(据白令安等,2012孙景贵等,2012陈衍景等,2012修改)

    Figure 4. 

    Distribution map of Early Mesozoic porphyry-type ore deposits in NE China (modified after Bai et al., 2012; Sun et al., 2012; Chen et al., 2012)

    图 5 

    东北地区早白垩世浅成热液矿床分布图(据白令安等,2012孙景贵等,2012Han et al., 2013; 陈衍景等,2012修改)

    Figure 5. 

    Distribution map of Early Cretaceous epithermal deposits in NE China (modified after Bai et al., 2012; Sun et al., 2012; Han et al., 2013; Chen et al., 2012)

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收稿日期:  2012-10-01
修回日期:  2013-01-02
刊出日期:  2013-02-01

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