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新疆尾亚地区石英二长闪长岩的岩浆混合成因

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文章导航 > 岩石学报 > 2007 > 23(4): 733-746
王玉往 王京彬 王莉娟 方同辉. 新疆尾亚地区石英二长闪长岩的岩浆混合成因[J]. 岩石学报, 2007, 23(4): 733-746.
引用本文: 王玉往 王京彬 王莉娟 方同辉. 新疆尾亚地区石英二长闪长岩的岩浆混合成因[J]. 岩石学报, 2007, 23(4): 733-746.
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Magma-mixing genesis of quartz monzodiorite in the Weiya, Xinjiang[J]. Acta Petrologica Sinica, 2007, 23(4): 733-746.
Citation: Magma-mixing genesis of quartz monzodiorite in the Weiya, Xinjiang[J]. Acta Petrologica Sinica, 2007, 23(4): 733-746.
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新疆尾亚地区石英二长闪长岩的岩浆混合成因

    • [1]中国地质大学（北京）中国地质大学地质过程与矿产资源国家重点实验室,北京100083 [2]中国科学院地质与地球物理所中国科学院矿产资源研究重点实验室,北京100029 [3]北京矿产地质研究院,北京100012

  • 基金项目:

    本文由中国地质大学地质过程与矿产资源国家重点实验室开放课题（GPMR0523）和国家重点基础研究发展计划（973计划）项目（2001CB409806）资助.致谢野外工作中得到新疆有色704地质队秦全新高级工程师及其尾亚项目组的大力支持,中国有色地质调查中心高珍全博士、中国科学院地质与地球物理研究所程春博士参加了部分野外工作.感谢与中国地质大学罗照华教授、莫宣学教授的有益讨论.

Magma-mixing genesis of quartz monzodiorite in the Weiya, Xinjiang

    • 1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geoscienees, Beijing 100083, China; 2. Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Scicnees, Beijing 100029, China ;3. Belling Institute of Geology for Mineral Resources, Beijing 100012, China

    摘要
  • 新疆东天山的尾亚钒钛磁铁矿矿区,在花岗岩中含有大量闪长岩包体,而且花岗岩与闪长岩相互包裹、渗透,并在花岗岩与闪长岩接触带形成二者混合的产物--岩浆混合岩.通过野外特征、岩相学和矿物成分对比,发现矿区中部的石英二长闪长（斑）岩体与岩浆混合岩完全相同,表明该岩体系岩浆混合成因.各类参与岩浆混合作用岩石的岩相学和矿物学表现出典型的岩浆混合作用特征.矿物不平衡组构主要有：钾长石的更长环斑结构、斑晶的环边结构、针状磷灰石发育、暗色矿物的聚晶团块、岩浆混合岩中出现钾长石“变晶”等等.各类岩石中斜长石和角闪石的主要氧化物成分对SiO2（%）表现出类似全岩哈克图解的线性关系.主要造岩矿物的化学成分以及钾长石巨晶的化学成分剖面,反映出本区岩浆混合作用有化学混合的参与.黑云母的化学成分表明,本区岩浆混合为以壳慢混源为基础的混合作用.
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修回日期:  2006-08-04
刊出日期:  2007-04-30

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