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中国蓝片岩带的分布及其构造意义

代艳娟 曾普胜 麻菁 苟瑞涛 王聚杰

代艳娟, 曾普胜, 麻菁, 等, 2015. 中国蓝片岩带的分布及其构造意义. 地质力学学报, 21 (3): 426-437.
引用本文: 代艳娟, 曾普胜, 麻菁, 等, 2015. 中国蓝片岩带的分布及其构造意义. 地质力学学报, 21 (3): 426-437.
ZENG Pu-sheng, ZENG Pu-sheng, MA Jing, et al., 2015. BLUESCHIST BELT IN CHINA AND ITS TECTONIC SIGNIFICANCE. Journal of Geomechanics, 21 (3): 426-437.
Citation: ZENG Pu-sheng, ZENG Pu-sheng, MA Jing, et al., 2015. BLUESCHIST BELT IN CHINA AND ITS TECTONIC SIGNIFICANCE. Journal of Geomechanics, 21 (3): 426-437.

中国蓝片岩带的分布及其构造意义

基金项目: 

国土资源大调查项目 12120113002500

国土资源部公益性行业科研专项 201211078

国家自然科学基金项目 41072073

详细信息
    作者简介:

    代艳娟(1990-), 女, 硕士研究生, 主要研究方向为矿床学、岩石学。E-mail:dyj4845121@foxmail.com

    通讯作者:

    曾普胜(1964-), 男, 博士, 研究员, 长期从事矿床学、岩石学和地球化学研究。E-mail:zengpusheng@vip.sohu.com

  • 中图分类号: P588.3

BLUESCHIST BELT IN CHINA AND ITS TECTONIC SIGNIFICANCE

  • 摘要: 在前人研究的基础上, 根据变质时代及产地将中国蓝片岩带划分为20个带, 选取不同时代典型蓝片岩带论述其特征(分布区域、大体规模、原岩特征、形成时代及矿物组合), 并对其地质成因进行分析。中国蓝片岩带生成方式复杂, 但均与俯冲消减作用有关, 且大多属B型俯冲消减; 部分地段叠加了A型俯冲的高压—超高压变质带(如阿尔金带、大别-苏北带、南迦巴瓦-密支那带等)。中国蓝片岩带在时代上可以分为元古代(晋宁期)、古生代(加里东—海西期)、中生代(印支—燕山期)和新生代(喜马拉雅期)4个时期, 每个时期蓝片岩带的形成大多与中国地体增生过程中洋盆的消减俯冲有关, 并在特定地段经历后期的陆内俯冲(高压—超高压俯冲)叠加影响。

     

  • 图  1  中国蓝片岩带分布简图(据Liou等[12];沈其韩等[11];李才等[21];魏永峰等[22],重新修编)

    1—扬子缝合带;2—兴凯(泛非)缝合带;3—加里东缝合带;4—华力西缝合带;5—印支缝合带;6—燕山缝合带;7—喜马拉雅缝合带;8—断裂;9—主要地质界线;10—榴辉岩;11—地体及编号:QL—祁连地体;QDM—柴达木地体;QT—羌塘地体;HL—喜马拉雅地体;WQ—西秦岭造山带;12—蓝片岩带及其编号:(1) 新疆唐巴勒-艾比湖蓝片岩带;(2) 新疆西南天山蓝片岩与超高压榴辉岩带的复合带;(3) 新疆南天山库米什蓝片岩带;(4) 新疆阿克苏蓝片岩带;(5) 内蒙古温都尔庙蓝片岩带;(6) 贺根山-苏尼特左旗蓝片岩带;(7) 北阿尔金蓝片岩带;(8) 祁连山蓝片岩带;(9) 西秦岭蓝片岩带;(10) 东秦岭-桐柏-大别蓝片岩带;(11) 苏北蓝片岩带;(12) 黑龙江牡丹江-依兰-萝北蓝片岩带;(13) 甘孜-理塘结合带;(14) 金沙江-哀牢山蓝片岩带;(15) 西藏羌塘龙木措-双湖蓝片岩带;(16) 滇西南澜沧江南段蓝片岩带;(17) 西藏雅鲁藏布江蓝片岩带;(18) 南迦巴瓦榴辉岩蓝片岩带;(19) 赣东北德兴-弋阳蓝片岩带;(20) 台湾玉里蓝片岩带

    Figure  1.  Simplified map of distribution of major blueschist zone in China

    表  1  几种蓝片岩相划分方案对比[3]

    Table  1.   Contrast of several dividing schemes of blueschist facies

    Bailey[16]Turner[18]Winkler[19]董申保[5~6]Liou等[20]
    蓝片岩相Law-Ab-Chl相Law带(很低级)蓝闪
    石片
    岩相
    蓝闪石-硬柱石
    片岩相
    蓝片岩相Law带
    蓝片岩相Gln+Law
    Gln+Omp
    或Gln+Jd+Q
    Law+Gln带(很低级)Pmp带
    Jd+Q(很低级)Ep带
    绿片岩相绿片岩相Gln+Czo带(低级)蓝闪绿片岩相
        注:矿物代号见正文后说明
    下载: 导出CSV

    表  2  中国蓝片岩时空分布特征

    Table  2.   Features of temporal-spatial distribution of blueschists in China

    高压变质带蓝片岩带位置及编号原岩
    类型
    典型高压
    变质矿物
    蓝片岩相平衡
    矿物共生组合
    变质相年代/Ma资料来源
    元古代
    天山褶皱带新疆阿克苏(4)1Cro、BarB1100Liou等[23]
    江南隆起
    西缘
    江西德兴
    (赣东北德兴-弋阳)(19)
    3Cro、JdA864.5±19
    867.5±13.5
    苏良树等[24]
    路台北缘
    高压变质带
    古生代(加里东—海西期)
    新疆南天山库米什(3)1Gln、CroⅡ,ⅢA350高俊等[25]
    新疆西天山特克斯(2)1Gln、Cro、LawⅠ,Ⅲ,Ⅳ早:A
    晚:B
    408
    345
    高俊等[26]
    北阿尔金(7)3Gln、Law、Phe、B490~515张建新等[27]
    内蒙古温都尔庙(5)2Gln、Law、AragⅠ,Ⅲ,ⅤA426±15王秉方[28]
    贺根山-苏尼特左旗(6)1Gln、CroⅡ,ⅢB400包志伟等[29]
    新疆唐巴勒-艾比湖(1)2Gln、CroⅡ,ⅢB450~475张立飞[30]
    华中高压
    变质带
    祁连山(8)1Gln、Cro、
    Jd、Arag
    Ⅰ,Ⅱ,
    Ⅲ,Ⅴ
    早:B
    中:A
    晚:B
    406~454
    420~490
    415±7
    吴汉泉[31]
    宋述光[32]
    林宜慧等[33]
    中生代(印支—燕山期)
    西秦岭(9)2Gln、Cro、PieⅡ,Ⅳ,Ⅴ早:A
    晚:B
    东秦岭-桐柏-大别(10)3Cro、Pie、Na-AugⅡ,Ⅳ,ⅤB220葛宁洁等[34]
    黑龙江牡丹江-依兰-
    萝北(12)
    1GlnA210~250Zhou等[35]
    苏北(江苏北部)(11)1Cro、Jd、PieⅢⅣⅤA258许志琴[36]
    印度-喜马
    拉雅高压带
    甘孜-理塘(13)
    金沙江-哀牢山
    (墨江)(14)
    2Cro、Mri、GlnA240~210Liou等[23]
    莫宣学等[37]
    顾徳林等[38]
    沙绍礼[39]
    班公湖(西藏羌塘)(15)
    怒江、滇西澜沧江-昌宁-
    孟连(16)
    3Gln、Cro、
    Na-Aug、Law
    Ⅰ,Ⅱ,Ⅲ409~519
    193~260
    周维全等[40]
    彭兴阶[41]
    罗万林等[42]
    瞿明国[43]
    赵靖等[44]
    新生代(喜马拉雅期)
    雅鲁藏布江(17)2Gln、Jd、Law、
    Arag
    Ⅰ,ⅡB59李才等[21]
    南迦巴瓦(18)2GtB50张泽明等[45]
    环太平洋
    高压带
    台湾玉理(20)2Gln、CroⅡ,ⅣB9~14Liou等[23]
        原岩类型:1—基性火山岩、硅质岩;2—基性火山岩、硅质岩伴超基性岩;3—细碧角斑岩(中基性火山岩、碎屑岩)
        矿物共生组合:Ⅰ—Gln+Law+Chl+Jd+Ep±Arag;Ⅱ—Gln+Ep+Chl+Ab+Q;Ⅲ—Cro+Ep+Chl+Q±Act;Ⅳ—Cro+Ep+Chl+Q+Gt±Pie;Ⅴ—Omp+Gt+Gln;
        变质相:A—蓝闪-硬柱石片岩相;B—蓝闪绿片岩相
    下载: 导出CSV
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  • 收稿日期:  2015-03-26
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