西藏雅鲁藏布江缝合带西段南北亚带蛇绿岩的成因探讨

刘飞, 杨经绥, 连东洋, 赵慧, 张岚, 张利, 黄健. 西藏雅鲁藏布江缝合带西段南北亚带蛇绿岩的成因探讨[J]. 岩石学报, 2015, 31(12): 3609-3628.
引用本文: 刘飞, 杨经绥, 连东洋, 赵慧, 张岚, 张利, 黄健. 西藏雅鲁藏布江缝合带西段南北亚带蛇绿岩的成因探讨[J]. 岩石学报, 2015, 31(12): 3609-3628.
LIU Fei, YANG JingSui, LIAN DongYang, ZHAO Hui, ZHANG Lan, ZHANG Li, HUANG Jian. Genesis and characteristics of the western part of the Yarlung Zangbo ophiolites, Tibet[J]. Acta Petrologica Sinica, 2015, 31(12): 3609-3628.
Citation: LIU Fei, YANG JingSui, LIAN DongYang, ZHAO Hui, ZHANG Lan, ZHANG Li, HUANG Jian. Genesis and characteristics of the western part of the Yarlung Zangbo ophiolites, Tibet[J]. Acta Petrologica Sinica, 2015, 31(12): 3609-3628.

西藏雅鲁藏布江缝合带西段南北亚带蛇绿岩的成因探讨

  • 基金项目:

    本文受中国地质调查局地质调查项目(12120115026801、12120115027201、201511022)、国际科技合作专项(2014DFR21270)和国家重点实验室自主课题(Z1301-a20)联合资助.

Genesis and characteristics of the western part of the Yarlung Zangbo ophiolites, Tibet

  • 雅鲁藏布江蛇绿岩带自萨嘎以西分为达巴-休古嘎布(南亚带)和萨嘎-达机翁(北亚带)两个亚带,但两者的关系和构造环境还存在争论。本文在实测剖面的基础上,对比南北亚带蛇绿岩产出和岩石组成,以及对比基性岩脉和围岩方辉橄榄岩的地球化学和年代学特征,探讨两个带的关系和构造环境。北带错不扎、加纳崩和巴尔基性岩脉具有高Si、Al,低K、Ti、P特征,属钙碱性玄武质成分,锆石U-Pb年龄为125~128Ma;南亚带东波、普兰、休古嘎布基性岩具有高Mg、Ti,低Si、K特征,为低钾拉斑玄武质成分,锆石U-Pb年龄为120~130Ma。南北带基性岩具有类似产状和年代学,球粒陨石标准化曲线与N-MORB一致;N-MORB标准化蛛网图中显示Nb、Ta、Ti负异常,指示洋内俯冲带弧前或弧后环境。此外,两带基性岩围岩方辉橄榄岩中橄榄石、辉石、尖晶石具有类似的矿物成分特征,地球化学成分兼有弧前和深海地幔橄榄岩的特点,指示南北亚带蛇绿岩形成于俯冲带弧前环境。结合区域对比,南亚带蛇绿岩不发育沟-弧-盆体系,具有从北到南的构造侵位特征,南北亚带之间的仲巴微地体具有特提斯喜马拉雅的亲缘性,指示南北蛇绿岩亚带可能为相同大洋岩石圈的不同残余。
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出版历程
收稿日期:  2015-05-20
修回日期:  2015-09-15
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