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    东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程

    裴先治 李瑞保 李佐臣 刘成军 陈有炘 裴磊 刘战庆 陈国超 李小兵 王盟

    裴先治, 李瑞保, 李佐臣, 刘成军, 陈有炘, 裴磊, 刘战庆, 陈国超, 李小兵, 王盟, 2018. 东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程. 地球科学, 43(12): 4498-4520. doi: 10.3799/dqkx.2018.124
    引用本文: 裴先治, 李瑞保, 李佐臣, 刘成军, 陈有炘, 裴磊, 刘战庆, 陈国超, 李小兵, 王盟, 2018. 东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程. 地球科学, 43(12): 4498-4520. doi: 10.3799/dqkx.2018.124
    Pei Xianzhi, Li Ruibao, Li Zuochen, Liu Chengjun, Chen Youxin, Pei Lei, Liu Zhanqing, Chen Guochao, Li Xiaobing, Wang Meng, 2018. Composition Feature and Formation Process of Buqingshan Composite Accretionary Mélange Belt in Southern Margin of East Kunlun Orogen. Earth Science, 43(12): 4498-4520. doi: 10.3799/dqkx.2018.124
    Citation: Pei Xianzhi, Li Ruibao, Li Zuochen, Liu Chengjun, Chen Youxin, Pei Lei, Liu Zhanqing, Chen Guochao, Li Xiaobing, Wang Meng, 2018. Composition Feature and Formation Process of Buqingshan Composite Accretionary Mélange Belt in Southern Margin of East Kunlun Orogen. Earth Science, 43(12): 4498-4520. doi: 10.3799/dqkx.2018.124

    东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程

    doi: 10.3799/dqkx.2018.124
    基金项目: 

    中央高校基本科研业务费专项资金项目 310827161006

    中央高校基本科研业务费专项资金项目 310827161002

    中央高校基本科研业务费专项资金项目 CHD2011TD020

    中央高校基本科研业务费专项资金项目 2013G1271092

    中央高校基本科研业务费专项资金项目 310827173702

    国家自然科学基金项目 41172186

    中央高校基本科研业务费专项资金项目 2013G1271091

    青海省国土资源厅-中国铝业公司公益性区域地质矿产调查基金项目 200801

    国家自然科学基金项目 41472191

    国家自然科学基金项目 41502191

    详细信息
      作者简介:

      裴先治(1963-), 男, 教授, 主要从事构造地质学和区域地质学研究

    • 中图分类号: P548

    Composition Feature and Formation Process of Buqingshan Composite Accretionary Mélange Belt in Southern Margin of East Kunlun Orogen

    • 摘要: 为了研究东昆仑南缘布青山复合增生型构造混杂岩带的物质组成、构造属性及形成演化历史,在前人资料基础上从构造混杂岩带物质组成、形成时代、构造属性等方面对其进行综合研究.研究结果表明,布青山复合增生型构造混杂岩带是一条分隔东昆仑造山带与巴颜喀拉造山带的增生型构造边界,主要由元古代-古生代不同构造属性的大型构造混杂岩块与混杂基质组成.构造混杂岩块包括中元古代中深变质基底岩块(苦海岩群)、寒武纪蛇绿岩岩块、奥陶纪蛇绿岩岩块、石炭纪蛇绿岩岩块、石炭纪洋岛/海山玄武岩岩块、奥陶纪中酸性弧岩浆岩岩块、格曲组磨拉石沉积等.基质岩系主要为一套强烈构造变形的早中二叠世马尔争组浊积岩系.该混杂岩带记录了东昆仑南缘布青山地区东特提斯洋(布青山洋)自新元古代晚期开启以来,从晚寒武世-中三叠世长期持续向北的洋壳消减及俯冲增生过程,并于中三叠世晚期布青山洋消减完毕而使巴颜喀拉地块与东昆仑地块碰撞拼合.该次造山事件导致了不同类型、不同时代构造岩块与马尔争组浊积岩强烈混杂,最终形成了布青山复合增生型构造混杂岩的基本构造格架.

       

    • 图  1  东昆仑造山带大地构造图(a)和布青山构造混杂岩带地质简图(b)

      1.第四系;2.新近纪贵德群;3.三叠纪巴颜喀拉山群;4.中二叠世闹仓坚沟组;5.早三叠世洪水川组;6.晚二叠世格曲组;7.早中二叠世马尔争组;8.晚石炭世-早二叠世树维门科组; 9.晚石炭世浩特洛哇组;10.海山灰岩;11.海山玄武岩;12.新元古代万宝沟岩群;13.中元古代狼牙山组;14.中元古代苦海岩群;15.晚三叠世斑状花岗岩;16.晚兰叠世正长花岗岩;17.晚三叠世石英闪长岩;18.晚三叠世闪长岩(哥日卓托岩体);19.早三叠世花岗闪长岩;20.早三叠世英云闪长岩;21.晚石炭世花岗闪长岩;22.石炭纪辉长岩+玄武岩;23.志留纪花岗闪长岩;24.志留纪英安岩;25.中奥陶世黑云母英云闪长岩;26.中奥陶世片麻状闪长岩;27.中奥陶世花岗闪长岩;28.中元古代英云闪长岩;29.石炭纪蛇绿岩组合;30.奥陶纪蛇绿岩沮合;31.奥陶纪辉长岩+玄武岩;32.奥陶纪蛇纹岩;33.寒武纪辉长岩+玄武岩;34.寒武纪蛇纹岩;35.时代不明蛇绿岩组合;36.实测地质界线;37.角度不整合;38.平行不整合;39.涌动接触;40.正常地层(层理)产状;41.倒转地层产状;42.片理产状;43.片麻理产状;44.正断层产状;45.逆断层产状;46.逆冲推覆断层;47.第四纪活动断层;48.水系

      Fig.  1.  Simplified tectonic framework of East Kunlun orogen (a) and geological map of Buqingshan tectonic melange belt (b)

      图  2  布青山地区地质简图

      1.第四系;2.晚二叠世格曲组;3.早中二叠世马尔争组;4.晚石炭世-早二叠世树维门科组;5.中元古代苦海岩群;6.硅泥质岩;7.海山灰岩;8.海山玄武岩;9.晚三叠世花岗闪长岩;10.石炭纪玄武岩;11.石炭纪辉长岩;12.石炭纪蛇纹岩;13.奥陶纪玄武岩;14.奥陶纪辉长岩;15.奥陶纪蛇纹岩;16.志留纪花岗闪长岩;17.志留纪英安岩;18.寒武纪玄武岩;19.寒武纪辉长岩;20.寒武纪蛇纹岩;21.地质界线;22.逆断层;23.推覆断层;24.层理及产状;25.实测剖面位置

      Fig.  2.  Simplified geological map of Buqingshan area

      图  3  东昆仑南缘布青山地区得力斯坦蛇绿岩(a)和哈尔郭勒西蛇绿岩(b)地质剖面

      1.硅泥质岩;2.长石石英岩屑砂岩;3.粗砾岩;4.钙质砾岩;5.似斑状黑云母花岗闪长岩;6.辉长岩;7.辉绿岩;8.玄武岩;9.角砾状玄武岩;10.蛇纹岩;11.辉绿岩脉;12.大理岩;13.产状;14.断层

      Fig.  3.  Geological section of Delisitan ophiolite (a) and Haerguolexi ophiolite (b) of Buqingshan area in southern East Kunlun

      图  4  东昆仑南缘可可尔塔地区蛇绿构造混杂岩地质简图

      1.第四系;2.晚石炭世浩特洛哇组;3.早中二叠世马尔争组;4.晚二叠世格曲组;5.晚石炭世-早中二叠世树维门科组;6.中元古代苦海岩群;7.志留纪花岗闪长岩;8.石炭纪蛇纹岩;9.石炭纪辉长岩;10.石炭纪玄武岩;11.奥陶纪蛇纹岩;12.奥陶纪辉长岩;13.奥陶纪玄武岩;14.寒武纪蛇纹岩; 15.寒武纪辉长岩及辉绿玢岩; 16.寒武纪玄武岩;17.剖面代号;18.断层;19.逆冲推覆断层;20.区域断裂;21.水系

      Fig.  4.  Simplified geological map of Kekeerta ophiolite in southern East Kunlun

      图  5  东昆仑南缘可可尔塔地区蛇绿混杂岩地质剖面

      AB.禾日沟贡玛地区蛇绿岩剖面;CD.可可尔塔地区蛇绿岩剖面.1.角砾状灰岩;2.粉砂质泥岩;3.炭质板岩;4.斜长角闪岩;5.石英岩;6.花岗岩;7.蛇纹岩;8.辉绿岩;9.辉长岩;10.斜长岩;11.地层产状;12.断裂

      Fig.  5.  Geological sections of Kekeerta ophiolite in southern East Kunlun

      图  6  东昆仑南缘布青山地区哈尔郭勒东蛇绿岩地质剖面

      1.硅泥质岩;2.含砾岩屑砂岩;3.中细粒辉长岩;4.辉绿岩;5.玄武岩;6.蛇纹岩;7.绿帘长石石英变粒岩;8.长石石英岩;9.蛇纹石化菱镁矿化大理岩;10.厚层块状大理岩;11.断层

      Fig.  6.  Geological section of Haerguoledong ophiolite of Buqingshan area in southern East Kunlun

      图  7  布青山构造混杂岩带不同类型洋岛/海山玄武岩地质简图

      1.第四系;2.早三叠世洪水川组;3.早中二叠世马尔争组;4.晚二叠世格曲组;5.晚石炭世浩特洛洼组;6.晚石炭世-早二叠世树维门科组;7.中元古代苦海岩群;8.晚三叠世花岗闪长岩;9.石炭纪玄武岩与辉长岩;10.奥陶纪玄武岩与辉长岩/寒武纪玄武岩与辉长岩;11.石炭纪蛇绿岩组合/奥陶纪蛇绿岩组合;12.奥陶纪辉橄岩/寒武纪辉橄岩;13.英安斑岩;14.洋岛/海山玄武岩;15.厚层块状碳酸盐岩;16.地质界线;17.角度不整合界线;18.区域边界断层/一般断层;19.逆冲推覆构造;20.地层产状;21.水系

      Fig.  7.  Simplified geological map of different types of oceanic island basalts in Buqingshan area

      图  8  布青山地区得力斯坦洋岛/海山玄武岩综合地层柱状图

      Fig.  8.  Comprehensive stratigraphic column of Delisitan seamount basalts in Buqingshan area

      图  9  布青山洋古生代-早中生代构造演化模式

      BB.巴颜喀拉地块;SKB.东昆南地体;NKB.东昆北地体;QB.柴达木地块

      Fig.  9.  Tectonic evolution cartoon of Buqingshan Ocean in Paleozoic-Early Mesozoic

      表  1  布青山构造混杂岩带物质组成

      Table  1.   Compositions of Buqingshan tectonic melange belt

      布青山复合增生型结构混杂岩带物质组成 类型 构造环境 物质组成 形成时化 代表性地质体 同位素年龄
      构造混杂岩 基质岩系 浊积岩相 马尔争姐 早中二叠世 马尔争姐浊积岩系 最小峰值年龄:421 Ma
      (未刊资料)
      磨拉石相 格曲組 晚二叠世 格曲组砂砾岩 最小峰值年龄:426 Ma
      (杨森等,2016)
      混杂岩块 变质基底 苦海岩群 中元古代 苦海岩群(变质岩块)
      洋壳型 寒武纪蛇绿岩 早寒武世 得力斯坦蛇绿岩 辉长岩:516.4±6.3Ma
      (刘战庆等,2011c)
      奥陶纪蛇绿岩 中晚奥陶世 哈尔郭勒西蛇绿岩 辉长岩:450±2Ma
      (未刊资料)
      禾日沟贡玛蛇绿岩 辉长岩:467±4Ma
      (未刊资料)
      可可尔塔蛇绿岩 辉长岩:457±2Ma
      斜长岩;452±9Ma
      (未刊资料)
      石炭纪蛇绿岩 早石炭世 哈尔郭勒东蛇绿岩 辉长若:332.8±3.1Ma
      (刘战庆等,2011c)
      洋岛海山玄武
      岩/灰岩组合
      石炭纪-二叠纪 得力斯坦南玄武岩 玄武岩:340.8±2.8Ma
      (杨杰等,2014)
      哈尔郭勒南玄武岩/灰岩组合
      哥日卓托南玄武岩/灰岩组合
      玄武岩/安山岩组合 禾日沟贡玛玄武岩/安山岩组合
      花岗闪长岩 早奥陶世早志留世 白日切特花岗闪长岩 花岗岩:439.0±1.9Ma
      (刘战庆等,2011a)
      亿可哈拉尔花岗闪长岩 花岗岩:436.4±6.8Ma
      花岗岩:436.9±5.7 Ma
      (Li et al., 2015)
      玛尼特花岗闪长岩 花岗岩:479±2Ma
      花岗岩:487±12Ma
      (Li et al., 2015)
      中酸性火山烙岩 早志留世 白日切特中酸性火山岩 英安岩:437.7±2.8Ma
      (刘战庆等,2011a)
      外来推覆体 台地相 树维口科组生物礁灰岩 晚石炭世早中二叠世 树维口科组(生物礁灰岩組合)
      钉合岩体 后碰撞型 闪长岩体 晚三叠世 哥日卓托闪长岩体 闪长岩:225.8±1.5Ma
      (李佐臣等,2013)
      下载: 导出CSV
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