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    山东省中部上寒武统碳酸盐风暴沉积的综合模式

    王家豪 王华 曾劲彪 程海

    王家豪, 王华, 曾劲彪, 程海, 2017. 山东省中部上寒武统碳酸盐风暴沉积的综合模式. 地球科学, 42(1): 68-77. doi: 10.3799/dqkx.2017.005
    引用本文: 王家豪, 王华, 曾劲彪, 程海, 2017. 山东省中部上寒武统碳酸盐风暴沉积的综合模式. 地球科学, 42(1): 68-77. doi: 10.3799/dqkx.2017.005
    Wang Jiahao, Wang Hua, Zeng Jinbiao, Cheng Hai, 2017. Integrative Depositional Model for Carbonate Tempestites in Upper Cambrian, Central Shandong Province. Earth Science, 42(1): 68-77. doi: 10.3799/dqkx.2017.005
    Citation: Wang Jiahao, Wang Hua, Zeng Jinbiao, Cheng Hai, 2017. Integrative Depositional Model for Carbonate Tempestites in Upper Cambrian, Central Shandong Province. Earth Science, 42(1): 68-77. doi: 10.3799/dqkx.2017.005

    山东省中部上寒武统碳酸盐风暴沉积的综合模式

    doi: 10.3799/dqkx.2017.005
    基金项目: 

    国家重大专项大型油气田及煤层气开发子课题 2016ZX05026-003-004

    详细信息
      作者简介:

      王家豪(1968-),副教授,博士,主要从事沉积-层序地层学科研和教学工作.ORCID: 0000-0003-1320-6852.E-mail:cugwangjiahao@163.com

    • 中图分类号: P5

    Integrative Depositional Model for Carbonate Tempestites in Upper Cambrian, Central Shandong Province

    • 摘要: 我国的碳酸盐风暴岩丰富多样,但前人对不同环境风暴岩的沉积作用、沉积序列和沉积模式的总结还不够完善.山东省中部上寒武统炒米店组碳酸盐风暴岩发育频繁,分布广,提供了全面分析风暴沉积作用的理想场所.基于该区详实的露头观察,可识别出冲刷面、渠模、丘状交错层理等典型的风暴沉积构造,以及砾屑灰岩、递变层理含砾砂屑灰岩-砂屑灰岩、纹层状粉-砂屑灰岩等风暴岩类型.根据砾屑颜色、磨圆度、排列方式、支撑结构、充填物等岩石学特征,研究区首要发育的砾屑灰岩可被细分为紧密堆积棱角状砾屑灰岩、基质支撑砾屑灰岩、砂屑支撑砾屑灰岩、水平-叠瓦状砾屑灰岩和放射状排列砾屑灰岩5种岩相类型,其分别归属于台前缓坡带原地-近源堆积、碎屑流、高密度-低密度浊流、风暴砾滩和风暴涡流沉积.对台前缓坡、台地边缘和开阔台地等不同环境的风暴沉积序列进行了归纳,建立了缓坡型碳酸盐台地风暴沉积的综合模式,并指出研究区频繁的风暴作用与全球气候变暖、海平面上升以及地震活动存在密切联系.研究表明较多台地边缘发育的大型渠模构造,其充填砾屑呈放射状排列,指示了渠模的风暴涡流成因

       

    • 图  1  山东省中部风暴沉积露头位置

      Fig.  1.  Outcrops sites of carbonate tempestites in the central Shandong Province

      图  2  山东省中部中-上寒武统岩性组成及沉积相演化

      Fig.  2.  Lithologic associations and sedimentary facies evolutions in the Middle to Upper Cambrian,central Shandong Province

      图  3  山东省中部中-上寒武统岩性组合露头

      a.大寺山露头,三山子组C段底部灰白色窝卷状叠层石白云岩;b.郭家庄露头,炒米店组上部灰白色厚层状白云质灰岩;c.郭家庄露头,炒米店组上部灰色波状层理灰岩及灰白色中厚层状白云质灰岩;d.张庄村露头,炒米店组上部灰色波状层理灰岩;e.郭家庄露头,炒米店组中部页岩夹薄层灰岩及透镜状砾屑灰岩;f.郭家庄露头,炒米店组下部页岩夹透镜状砾屑灰岩;g.柳条峪村露头,崮山组灰色页岩夹少量链条状、薄层状灰岩;h.柳条峪村露头,张夏组上灰岩段叠层石灰岩

      Fig.  3.  Outcrop sceneries showing the lithologic associations in the Middle to the Upper Cambrian,central Shandong Province

      图  4  冲刷面和渠模构造

      a.大寺山露头,冲刷面、砾屑灰岩和丘状交错层理砂屑灰岩构成的垂向序列;b.张家庄露头,砾屑灰岩、薄层状灰岩及渠模构造;c.张庄村露头,正常天气灰色薄层状灰岩及渠模、纹层状砂屑灰岩;d.郭家庄露头,灰白色碎裂状白云质灰岩及渠模构造;e.郭家庄露头,渠模及充填砾屑灰岩、叠瓦状灰岩;f.郭家庄露头,水平-叠瓦状砾屑灰岩及渠模构造.红色点线和红色箭头指示渠模构造,向上的三角形示意单个风暴沉积序列

      Fig.  4.  Sedimentary structures of scouring surface and gutter cast

      图  5  砾屑灰岩岩相类型

      a.张庄村露头,紧密堆积棱角状砾屑灰岩相以及平行层理砂屑灰岩、渠模;b.郭家庄露头,紧密堆积棱角状砾屑灰岩相及纹层粉屑灰岩;c.张庄村露头,基质支撑砾屑灰岩相;d.大寺山露头,砂屑支撑砾屑灰岩相

      Fig.  5.  Lithofacies types of calcirudite

      图  6  砾屑灰岩岩相类型

      a,b.大寺山露头,冲刷面、砾屑灰岩、递变砂屑灰岩及纹层状砂屑灰岩构成的风暴沉积序列;c,d.张庄村露头,叠瓦状砾屑灰岩;g,h.张庄村露头,反射状、水平-叠瓦状砾屑灰岩;e,f.郭家庄露头,灰色薄层灰岩夹放射状砾屑灰岩

      Fig.  6.  Lithofacies types of calcirudite

      图  7  递变灰岩、纹层状灰岩及风暴沉积序列

      a,b.郭家庄剖面,水平-叠瓦状砾屑灰岩、含砾砂屑灰岩及丘状交错层理砂屑灰岩构成的风暴沉积序列;c.郭家庄剖面,砾屑灰岩、含砾砂屑灰岩丘状交错层理砂屑灰岩构成的风暴沉积序列;d.郭家庄剖面,多期叠置的水平砾屑灰岩

      Fig.  7.  Graded calcarenite,laminated calcarenite and vertical successions of storm deposits

      图  8  缓坡型台地碳酸盐风暴沉积的综合模式和典型沉积序列

      Fig.  8.  Integrative model for carbonate storm deposits and typical depositional successions at a ramp platform

      图  9  炒米店组上部碎裂状白云质灰岩及漏斗状裂缝

      照片来自郭家庄露头

      Fig.  9.  Funnel-shaped cracks in fragmental dolomitized limestone of the upper Chaomidian Formation

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