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大同地区早中生代煌斑岩—碳酸岩岩墙群

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文章导航 > 岩石学报 > 2003 > 19(1): 93-104

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邵济安 张永北 等. 大同地区早中生代煌斑岩—碳酸岩岩墙群[J]. 岩石学报, 2003, 19(1): 93-104.
引用本文: 邵济安 张永北 等. 大同地区早中生代煌斑岩—碳酸岩岩墙群[J]. 岩石学报, 2003, 19(1): 93-104.
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SHAO JiAn,ZHANG YongBei,ZHANG LuQiao,MU BaoLei,WANG PeiYing and GUO Feng. Early Mesozoic dike swarms of carbonatites and lamprophyres in Datong area[J]. Acta Petrologica Sinica, 2003, 19(1): 93-104.
Citation: SHAO JiAn,ZHANG YongBei,ZHANG LuQiao,MU BaoLei,WANG PeiYing and GUO Feng. Early Mesozoic dike swarms of carbonatites and lamprophyres in Datong area[J]. Acta Petrologica Sinica, 2003, 19(1): 93-104.
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大同地区早中生代煌斑岩—碳酸岩岩墙群

    • [1]北京大学地球与空间科学学院，北京100871 [2]中国科学院地质地球物理研究所，北京100029

  • 基金项目:

    国家自然科学基金(批准号49872079,40072073)，中科院知识创新工程项目(KZCX1-07)

Early Mesozoic dike swarms of carbonatites and lamprophyres in Datong area

    • 1. Department of Geology,Peking University,Beijing 100871,China; 2. Institute of Geology and Geophysics,Chnese Academy of Sciences,Beijing 100029,China; 3. Geological Burean of Inner Mongolia,Huhhot 010020,China; 4. Changsha Institute of Geotectonics,Chinese Academy of Sciences,Changsha 410013,China

    摘要
  • 大同地区密集分布的岩墙群由基性－超基性煌斑岩和碳酸岩组成，侵入石炭－二叠纪煤层中。与地层的接触关系和Rb-Sr,K-Ar同位素年代学数据表明墙群的侵位于晚三叠世。Sr,Nd同位素比值显示，碳酸岩和煌斑岩都来源于壳幔混合型岩浆源区。稳定元素比值和相容，不相容元素同等富集则表明是碳酸岩和硅酸盐混合的原始母岩浆液态不混熔的产物。 岩墙群形成的地质条件和构造背景表明，它们是在伸展构造背景下，受到不同级别的构造控制，大同岩墙群的研究对进一步认识华北早中生代岩石圈演化有重要的意义。
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修回日期:  2002-07-16
刊出日期:  2003-02-28

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