柴北缘超高压变质带的新元古代变质作用——来自锡铁山副片麻岩的岩石学及独居石年代学证据

张聪, 刘晓瑜, 杨经绥, 李鹏, 张立飞. 柴北缘超高压变质带的新元古代变质作用——来自锡铁山副片麻岩的岩石学及独居石年代学证据[J]. 岩石学报, 2016, 32(12): 3715-3728.
引用本文: 张聪, 刘晓瑜, 杨经绥, 李鹏, 张立飞. 柴北缘超高压变质带的新元古代变质作用——来自锡铁山副片麻岩的岩石学及独居石年代学证据[J]. 岩石学报, 2016, 32(12): 3715-3728.
ZHANG Cong, LIU XiaoYu, YANG JingSui, LI Peng, ZHANG LiFei. The Neoproterozoic metamorphism of North Qaidam UHPM belt, western China: Constrain from petrological study and monazite dating of paragneiss[J]. Acta Petrologica Sinica, 2016, 32(12): 3715-3728.
Citation: ZHANG Cong, LIU XiaoYu, YANG JingSui, LI Peng, ZHANG LiFei. The Neoproterozoic metamorphism of North Qaidam UHPM belt, western China: Constrain from petrological study and monazite dating of paragneiss[J]. Acta Petrologica Sinica, 2016, 32(12): 3715-3728.

柴北缘超高压变质带的新元古代变质作用——来自锡铁山副片麻岩的岩石学及独居石年代学证据

  • 基金项目:

    本文受国家自然科学基金项目(41572051)、中国地质科学院地质研究所基本科研业务费(J1518)和中国地质调查项目(DD20160022-01)联合资助.

The Neoproterozoic metamorphism of North Qaidam UHPM belt, western China: Constrain from petrological study and monazite dating of paragneiss

  • 同一造山带中所包含的多期造山作用信息是研究不同时代区域构造演化的重要依据,对理解不同时期造山过程中岩石组合及其地球化学演化有重要的指示意义。但由于晚期造山作用往往会部分或者完全抹除岩石中保存的早期造山作用信息,使得对记录多期造山作用的岩石中早期造山带变质作用及年代学信息的研究变得十分困难。独居石为一种副变质岩中的常见副矿物,由于其具有很高的U-Th-Pb体系封闭温度和对流体及变质温压条件的敏感性,使其可以记录多期造山过程中丰富的年代学信息。电子探针独居石原位化学定年方法使得年代学信息与岩石中矿物学信息及变质反应相联系,从而得到不同时期岩石记录的P-T-t轨迹。我们利用独居石电子探针原位U-Th-Pb定年手段与岩石学研究相结合的方法,在柴北缘早古生代加里东期超高压变质带锡铁山地区的含石榴石蓝晶石/夕线石黑云斜长片麻岩基质矿物及石榴石变斑晶的独居石中获得886±18Ma格林威尔期的年龄等时线。独居石稀土元素配分特征与新元古代变质独居石相吻合。通过传统矿物对温压计计算得到格林威尔期现存矿物组合记录了高角闪岩相变质温压条件607~727℃,6.5~10.0kbar,略高于区内记录古生代变质作用的副片麻岩。与记录古生代加里东期变质年龄的副片麻岩相比,格林威尔期副片麻岩在微量元素地球化学上具有高的稀土总量和明显的Eu的负异常特点(Eu/Eu*=0.50),并相应的亏损Ba、Sr元素,表现出活动大陆边缘沉积岩的地球化学特征。结合全球格林威尔期造山事件及罗迪尼亚超大陆的形成及裂解过程,我们认为柴北缘地区在新元古代时期应为与罗迪尼亚超大陆形成有关的活动大陆边缘地区。
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收稿日期:  2016-05-03
修回日期:  2016-08-19
刊出日期:  2016-12-31

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