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准噶尔盆地北三台凸起断裂结构特征及成岩封闭作用

张丽辰 吴孔友 何文军 陈洪 郑孟林 贾西玉

张丽辰, 吴孔友, 何文军, 等, 2018. 准噶尔盆地北三台凸起断裂结构特征及成岩封闭作用. 地质力学学报, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061
引用本文: 张丽辰, 吴孔友, 何文军, 等, 2018. 准噶尔盆地北三台凸起断裂结构特征及成岩封闭作用. 地质力学学报, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061
ZHANG Lichen, WU Kongyou, HE Wenjun, et al., 2018. STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN. Journal of Geomechanics, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061
Citation: ZHANG Lichen, WU Kongyou, HE Wenjun, et al., 2018. STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN. Journal of Geomechanics, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061

准噶尔盆地北三台凸起断裂结构特征及成岩封闭作用

doi: 10.12090/j.issn.1006-6616.2018.24.05.061
基金项目: 

国家自然科学基金 41272142

详细信息
    作者简介:

    张丽辰(1991-), 女, 硕士, 研究方向构造地质学。E-mail:1226401705@qq.com

    通讯作者:

    吴孔友(1971-), 男, 博士, 教授, 主要从事地质构造与油气成藏研究。E-mail:wukongyou@163.com

  • 中图分类号: P542.3;P618.13

STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN

  • 摘要: 断层具有复杂的内部结构,可划分为滑动破碎带和诱导裂缝带两个结构单元。断裂带内部成岩作用普遍发育,其中,胶结作用是断裂两侧诱导裂缝带中较常见的成岩作用,影响着断裂的垂向封闭性。利用地震、测井、岩心等资料定量化的对准噶尔盆地北三台凸起主要断裂进行结构划分,利用岩心、镜下薄片观察的方法研究断裂带成岩胶结作用。研究发现:断裂带成岩胶结作用显著,胶结物以方解石为主,还发现有粘土矿物、沸石、石英等胶结裂缝。大型主控断裂裂缝充填程度相比派生断裂高,胶结程度致密,对油气的封堵性能更强。通过镜下鉴定及流体包裹体均一温度测定发现:北三台凸起断裂带至少经历了3期大规模流体活动,多期的流体作用导致该区断裂的成岩封闭。

     

  • 图  1  研究区位置图

    Figure  1.  Location of the study area

    图  2  北三台凸起断层平面分布图

    Figure  2.  The planar distribution and structural characteristics of faults in the Beisantai swell

    图  3  西泉2井断裂带内部结构测井曲线综合判别图

    Figure  3.  Comprehensive discrimination of the internal structure of fault in well Xiquan 2

    图  4  断裂带内部结构发育规律

    a—滑动破碎带与诱导裂缝带关系;b—断裂带内部结构各部分占比;c—断距与断裂带宽度关系

    Figure  4.  The internal structure development regulation of the fault zone

    图  5  北三台凸起主干断层胶结物类型

    Figure  5.  Cement types of the main faults in the Beisantai swell

    图  6  断裂带内流体包裹体产状、形态特征

    Figure  6.  Fluid inclusion occurrences and characteristics in the fault zone

    图  7  北三台凸起断裂带流体活动史

    (a)流体包裹体均一温度分布直方图    (b)北13井埋藏史图

    Figure  7.  Fluid activity history of the fault zone in the Beisantai swell

    表  1  断裂带结构单元测井曲线识别判别标准表

    Table  1.   Well logging curve identification criterion of fault zone structure unit

    断裂结构单元 RTC P2 ΔAC ΔDEN ΔCNL CALd CWP
    滑动破碎带 稳定,值小,无差值 稳定、值较小 稳定、值较小 稳定、值较小 稳定、值较小 稳定、值较小 稳定、值较小
    诱导裂缝带 波动,值大,有差值 波动、值较大 波动、跳跃、较大 波动、值较大 波动、值较大 波动、值较大 波动、值较大
      注:RTC-深浅电阻率差比;P2-次生孔隙度变化值;ΔAC-声波变化率;ΔDEN-密度变化率;ΔCNL-中子变化率;CALd-井径增大率;CWP-断裂带综合判别参数
    下载: 导出CSV
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  • 收稿日期:  2017-12-12
  • 修回日期:  2018-04-08
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