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    南阿尔金陆块科克萨依新元古代花岗岩成因及地质意义

    陈红杰 吴才来 雷敏 郭文峰 张昕 郑坤 高栋 吴迪

    陈红杰, 吴才来, 雷敏, 郭文峰, 张昕, 郑坤, 高栋, 吴迪, 2018. 南阿尔金陆块科克萨依新元古代花岗岩成因及地质意义. 地球科学, 43(4): 1278-1292. doi: 10.3799/dqkx.2018.720
    引用本文: 陈红杰, 吴才来, 雷敏, 郭文峰, 张昕, 郑坤, 高栋, 吴迪, 2018. 南阿尔金陆块科克萨依新元古代花岗岩成因及地质意义. 地球科学, 43(4): 1278-1292. doi: 10.3799/dqkx.2018.720
    Chen Hongjie, Wu Cailai, Lei Min, Guo Wenfeng, Zhang Xin, Zheng Kun, Gao Dong, Wu Di, 2018. Petrogenesis and Implications for Neoproterozoic Granites in Kekesayi Area, South Altyn Continent. Earth Science, 43(4): 1278-1292. doi: 10.3799/dqkx.2018.720
    Citation: Chen Hongjie, Wu Cailai, Lei Min, Guo Wenfeng, Zhang Xin, Zheng Kun, Gao Dong, Wu Di, 2018. Petrogenesis and Implications for Neoproterozoic Granites in Kekesayi Area, South Altyn Continent. Earth Science, 43(4): 1278-1292. doi: 10.3799/dqkx.2018.720

    南阿尔金陆块科克萨依新元古代花岗岩成因及地质意义

    doi: 10.3799/dqkx.2018.720
    基金项目: 

    中国地质调查局项目 121201102000150005-06

    中国地质调查局项目 12120115027001

    国家自然科学基金项目 41272079

    详细信息
      作者简介:

      陈红杰(1985-), 男, 博士研究生, 矿物学、岩石学、矿床学专业

      通讯作者:

      吴才来

    • 中图分类号: P588.121;P597.3

    Petrogenesis and Implications for Neoproterozoic Granites in Kekesayi Area, South Altyn Continent

    • 摘要: 南阿尔金陆块是阿尔金造山带的重要组成部分.大量新元古代花岗岩出露于南阿尔金亚干布阳-帕夏拉依裆-科克萨依一带.这些花岗岩记录了与Rodinia超大陆汇聚有关的动力学信息,因此对其进行研究有利于对阿尔金造山带演化历史的认识和理解.选取了科克萨依花岗岩岩体进行了岩相学、地球化学、锆石U-Pb年代学和Hf同位素组成的研究.研究结果表明:(1)科克萨依二长花岗岩的主要矿物有:石英、钾长石、斜长石、黑云母和白云母;花岗岩的锆石U-Pb年龄为947~945 Ma.(2)地球化学特征显示,岩石具有高SiO2(71.54%~74.69%)、高Na2O+K2O(6.33%~7.40%),低CaO(1.59%~2.00%),低MgO(0.43%~0.61%)和TiO2(0.25%~0.37%)的特征,相对富钾,K2O/Na2O比值为1.02~1.71,A/CNK在1.10~1.14之间,属高钾钙碱性系列的过铝质花岗岩.富集Rb、Th、K、La等元素,亏损Nb、Ta、P、Ti等元素;轻稀土富集而重稀土亏损,具有明显的负Eu异常.(3)锆石εHft)为-4.09~+3.87之间,二阶段模式年龄tDM2为1.6~2.0 Ga.这些特征表明科克萨依二长花岗岩是古老地壳富长石贫黏土的(变)杂砂岩部分熔融形成的S型花岗岩.结合相邻地区新元古代花岗岩类的地球化学、同位素特征及阿尔金区域构造资料,认为科克萨依二长花岗岩形成于新元古代时期,是碰撞造山环境下的产物,是Rodinia超大陆汇聚碰撞过程的响应.

       

    • 图  1  阿尔金造山带地质图及研究区地质简图

      图a据Liu et al.(2012);b据吴才来等(2016);c据西安地质矿产研究所(2003)编新疆1:25万苏吾什杰幅区域地质调查报告.TRB.塔里木盆地;QL.祁连山;QDB.柴达木盆地;WKL.西昆仑;EKL.东昆仑;HMLY.喜马拉雅山

      Fig.  1.  Geological sketch map of Altyn Tagh orogenic belt and geological sketch map of study area

      图  2  科克萨依岩体野外及镜下照片

      a.科克萨依岩体野外露头;b.新元古代花岗岩野外露头;c, d.二长花岗岩镜下照片(正交偏光);Pl.斜长石;Mc.微斜长石;Qz.石英;Bi.黑云母;Ms.白云母

      Fig.  2.  Outcrops and photomicrographs of Kekesayi granite

      图  3  科克萨依新元古代花岗岩体全岩SiO2-Na2O+K2O (a),SiO2-K2O (b)和A/CNK-A/NK图解(c)

      图a据Maniar and Piccoli(1989);图b据Middlemost(1994);图c据Martin et al.(2005)

      Fig.  3.  Whole-rock SiO2 vs. Na2O+K2O classification diagram (a), SiO2 vs. K2O diagram (b) and A/CNK vs. A/NK diagram (c) of Kekesayi Neoproterozoic granites

      图  4  科克萨依花岗岩全岩稀土配分模式(a)和微量元素蛛网图(b)

      标准化值据Sun and McDonough(1989)

      Fig.  4.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized spider diagrams (b) for the granites in Kekesayi area

      图  5  科克萨依地区花岗岩体锆石谐和曲线

      Fig.  5.  Concordia plots of the granites in Kekesayi area

      图  6  科克萨依花岗岩体锆石Hf同位素组成

      Fig.  6.  Hf isotopic compositions of zircons from granites in Kekesayi area

      图  7  科克萨依地区花岗质岩体C/MF-A/MF图解(a),Al2O3+FeOT+MgO+TiO2-Al2O3/(FeOT+MgO+TiO2)图解(b),Al2O3/TiO2-CaO/Na2O图解(c)和Rb/Sr-Rb/Ba图解(d)

      图a据Alther et al.(2000);图b据Douce(1999);图d据Sylvester(1998).数据来源:Himalayan淡色花岗岩据Searle and Fryer(1986); Inger and Harris(1993); Ayres and Harris(1997).Lachlan S型花岗岩据Chappell and Simpson(1984); Healy et al.(2004)

      Fig.  7.  Geochemical diagrams of granites in Kekesayi area, C/MF vs. A/MF (a), Al2O3+FeOT+MgO+TiO2 vs. Al2O3/(FeOT+MgO+TiO2) (b), Al2O3/TiO2 vs. CaO/Na2O (c), Rb/Sr vs. Rb/Ba (d)

      图  8  Rb-Th图解(a)和CaO-FeOT+MgO-(Al2O3-(Na2O+K2O))图解(b)

      图a据Chappell et al.(1999);图b据White and Chappell(1977)

      Fig.  8.  Diagram of Rb-Th (a) and diagram of CaO-FeOT+MgO-(Al2O3-(Na2O+K2O))(b)

      图  9  岩石R1-R2构造环境判断图解(a)和岩石Nb-Y图解(b)

      图a底图据Batchelor and Bowden(1985);图b底图据Pearce et al.(1984).①地幔分异产物;②板块碰撞前;③碰撞隆起后;④造山晚期;⑤非造山;⑥同碰撞;⑦造山期后

      Fig.  9.  R1-R2 discrimination diagram (a) and Nb-Y diagram (b)

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