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    海拉尔盆地西部坳陷带侏罗系火山机构识别及发育特征

    赵德锋 史冠中 侯艳平 沈传波 吴路路 曾小伟 孙荣耀 郑晨宇 彭宇虓 陈鹏

    赵德锋, 史冠中, 侯艳平, 沈传波, 吴路路, 曾小伟, 孙荣耀, 郑晨宇, 彭宇虓, 陈鹏, 2023. 海拉尔盆地西部坳陷带侏罗系火山机构识别及发育特征. 地球科学, 48(4): 1517-1531. doi: 10.3799/dqkx.2022.081
    引用本文: 赵德锋, 史冠中, 侯艳平, 沈传波, 吴路路, 曾小伟, 孙荣耀, 郑晨宇, 彭宇虓, 陈鹏, 2023. 海拉尔盆地西部坳陷带侏罗系火山机构识别及发育特征. 地球科学, 48(4): 1517-1531. doi: 10.3799/dqkx.2022.081
    Zhao Defeng, Shi Guanzhong, Hou Yanping, Shen Chuanbo, Wu Lulu, Zeng Xiaowei, Sun Rongyao, Zheng Chenyu, Peng Yuxiao, Chen Peng, 2023. Identification and Developmental Characteristics of the Jurassic Volcanic Edifice in the Western Depression, Hailar Basin. Earth Science, 48(4): 1517-1531. doi: 10.3799/dqkx.2022.081
    Citation: Zhao Defeng, Shi Guanzhong, Hou Yanping, Shen Chuanbo, Wu Lulu, Zeng Xiaowei, Sun Rongyao, Zheng Chenyu, Peng Yuxiao, Chen Peng, 2023. Identification and Developmental Characteristics of the Jurassic Volcanic Edifice in the Western Depression, Hailar Basin. Earth Science, 48(4): 1517-1531. doi: 10.3799/dqkx.2022.081

    海拉尔盆地西部坳陷带侏罗系火山机构识别及发育特征

    doi: 10.3799/dqkx.2022.081
    基金项目: 

    湖北省自然科学基金创新群体项目 2021CFA031

    详细信息
      作者简介:

      赵德锋(1995-),男,硕士研究生,主要从事火山岩储层方面的研究.ORCID: 0000-0002-1094-2304. E-mail: cug_ZhaoDefeng@163.com

      通讯作者:

      沈传波,ORCID: 0000-0001-5641-9714. E-mail: cbshen@cug.edu.cn

    • 中图分类号: P545

    Identification and Developmental Characteristics of the Jurassic Volcanic Edifice in the Western Depression, Hailar Basin

    • 摘要: 火山岩型油气藏是当前油气勘探新领域,勘探实践表明海拉尔盆地侏罗纪火山-沉积地层具有良好的油气勘探前景.海拉尔盆地西部坳陷带分布在德尔布干断裂和额尔古纳断裂之间,断裂构造对火山喷发和盆地填充过程有重要的控制作用,然而断裂构造和火山岩相之间的耦合关系尚不明确,制约了该区火山岩型油气藏勘探部署.针对这一问题,利用钻井岩心、测录井和地震资料,运用井-震对比、多属性联合等方法,分析了西部坳陷带各类火山-沉积岩的测井特征和地震反射特征,识别火山机构并进行岩相古地理重建.研究表明,德尔布干和额尔古纳断裂带影响了中-晚侏罗世火山岩的横向展布,火山机构主要分布在凹陷缓坡带,在平面上沿NE向次级断裂呈串珠状、条带状分布,呈多中心复合式爆发样式.凹陷内平行断层组合、反向调节断层组合、断裂转折带、雁列式断层组合4种断裂组合对火山机构类型和发育有明显控制作用.沉积岩主要发育在火山与断裂围限的可容纳空间内,断裂与火山古地貌共同控制了凹陷内沉积砂体的展布.

       

    • 图  1  海拉尔盆地西部坳陷带区域地质概况图

      a.海拉尔盆地西部坳陷带区域位置图;断裂据张龙升等(2021)修改;b.海拉尔盆地西部坳陷带地震剖面图

      Fig.  1.  Overview of regional geology in western depression zone of Hailar basin

      图  2  巴彦呼舒凹陷火山岩性识别典型连井剖面

      Fig.  2.  Typical well connection profile on lithology identification of volcanics in Bayanhushu depression

      图  3  巴彦呼舒凹陷典型火山机构刻画

      剖面位置见图1B-B'

      Fig.  3.  Characterization of typical volcanic edifices in Bayanhushu depression

      图  4  巴彦呼舒凹陷火山-沉积相带预测

      a. 局部方差属性切片;b. 均方根振幅属性切片;c. 分频属性切片;d. 火山-沉积相带预测

      Fig.  4.  Prediction of volcanic and sedimentary facies belt in Bayanhushu depression

      图  5  海拉尔盆地西部坳陷带侏罗系断裂及火山-沉积岩相平面展布

      Fig.  5.  The plane distributive maps of the fault and volcanic or sedimentary lithofacies of the Jurassic strata in western depression zone of Hailar basin

      图  6  海拉尔盆地西部坳陷带侏罗系断裂特征剖面图

      a.巴彦呼舒凹陷断层样式;b.查干诺尔凹陷断层样式

      Fig.  6.  The characteristic maps of the faults of the Jurassic strata in western depression zone of Hailar basin

      图  7  海拉尔盆地西部坳陷带侏罗系次级断裂与火山沉积中心组合样式

      图a,b,c,d剖面位置见图5

      Fig.  7.  The association styles of secondary fault and volcanic apparatus center of the Jurassic strata in western depression zone of Hailar basin

      图  8  海拉尔盆地西部坳陷带缓坡带串珠状火山机构

      a.地震剖面;b.均方根振幅属性切片;剖面位置见图5A1-A2

      Fig.  8.  The beaded volcanic edifices of the gentle slope zone in the in western depression zone of Hailar basin

      图  9  海拉尔盆地西部坳陷带侏罗系火山沉积模式

      Fig.  9.  The Jurassic volcanic sedimentary pattern in the western depression zone of Hailar basin

      表  1  岩性对应地震反射特征及测井曲线特征

      Table  1.   Seismic reflection characteristics and logging curve characteristics corresponding to lithology

      岩性 地震反射特征 测井曲线特征
      振幅 频率 连续性 GR(API) RD(Ω·m)
      流纹岩、英安岩 中-强振幅 中-低频率 连续性差 132~206 10~158
      玄武岩和安山岩 强振幅 中-低频率 连续性好 39~120 <45
      凝灰岩 中等振幅 中-高频率 连续性较好 60~240 3~240
      火山角砾岩 中-强振幅 中-低频率 连续性差 >135 <30
      砂砾岩 弱振幅 中-低频率 连续性差 >126 <35
      泥岩、砂岩 中等振幅 中-高频率 连续性好 >105 <35
      下载: 导出CSV
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    • 收稿日期:  2022-01-18
    • 刊出日期:  2023-04-25

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