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莱南斜坡带沙四段—沙三下亚段原型盆地恢复及其对沉积的控制

王启明 黄晓波 周晓光 刘睿 李晓辉

王启明, 黄晓波, 周晓光, 等, 2018. 莱南斜坡带沙四段—沙三下亚段原型盆地恢复及其对沉积的控制. 地质力学学报, 24 (3): 371-380. DOI: 10.12090/j.issn.1006-6616.2018.24.03.038
引用本文: 王启明, 黄晓波, 周晓光, 等, 2018. 莱南斜坡带沙四段—沙三下亚段原型盆地恢复及其对沉积的控制. 地质力学学报, 24 (3): 371-380. DOI: 10.12090/j.issn.1006-6616.2018.24.03.038
WANG Qiming, HUANG Xiaobo, ZHOU Xiaoguang, et al., 2018. THE RECOVERY OF PROTOTYPE BASIN AND ITS CONTROL OVER THE DEPOSITION IN THE LOWER THIRD SUB-MEMBER AND FOURTH MEMBER OF THE SHAHEJIE FORMATION IN THE SOUTH SLOPE ZONE OF THE LAIZHOUWAN SAG. Journal of Geomechanics, 24 (3): 371-380. DOI: 10.12090/j.issn.1006-6616.2018.24.03.038
Citation: WANG Qiming, HUANG Xiaobo, ZHOU Xiaoguang, et al., 2018. THE RECOVERY OF PROTOTYPE BASIN AND ITS CONTROL OVER THE DEPOSITION IN THE LOWER THIRD SUB-MEMBER AND FOURTH MEMBER OF THE SHAHEJIE FORMATION IN THE SOUTH SLOPE ZONE OF THE LAIZHOUWAN SAG. Journal of Geomechanics, 24 (3): 371-380. DOI: 10.12090/j.issn.1006-6616.2018.24.03.038

莱南斜坡带沙四段—沙三下亚段原型盆地恢复及其对沉积的控制

doi: 10.12090/j.issn.1006-6616.2018.24.03.038
基金项目: 

“十三五”科技国家重大专项课题 2016ZX05024003

详细信息
    作者简介:

    王启明(1984-), 男, 硕士, 高级工程师, 主要从事油气勘探研究工作。E-mail:wangqm@cnooc.com.cn

  • 中图分类号: P618.13

THE RECOVERY OF PROTOTYPE BASIN AND ITS CONTROL OVER THE DEPOSITION IN THE LOWER THIRD SUB-MEMBER AND FOURTH MEMBER OF THE SHAHEJIE FORMATION IN THE SOUTH SLOPE ZONE OF THE LAIZHOUWAN SAG

  • 摘要: 莱州湾凹陷南部斜坡带后期经历多次大规模构造运动改造,导致原始盆地面貌不清,沉积体系分布不明确。以构造演化分析为主线,通过地震解释、声波时差法和趋势厚度法相结合,对沙河街组早期沙四段-沙三下亚段沉积时期的原型盆地面貌及其配置关系进行了恢复,并明确了不同沉积体系的平面分布及控制因素。研究表明:(1)沙四沉积时期,莱南斜坡带整体受断裂伸展活动引起的块体差异升降,西部受两组东西向断层分割形成3个东西向展布的断槽,东部及南部为潍北凸起的隆起区,早期断层分割东西古地貌变化;(2)沙三下沉积时期,整体快速沉降,西部受东西向断裂差异抬升,形成局部高地,潍北凸起东部一部分后期逐渐淹没于水下,形成宽缓台地背景;(3)不同物源体系供给控制了沙四段扇三角洲与辫状河三角洲差异分布,古地貌与物源差异供给共同控制了沙三下亚段湖相碳酸盐岩与风化残积相的发育与垂向分布。沉积体系的发育和分布对于盆地原型面貌具有重要的响应关系。

     

  • 图  1  莱州湾凹陷南部斜坡带区域位置

    Figure  1.  Regional location of the south slope zone of the Laizhouwan Sag

    图  2  莱州湾凹陷南部斜坡带典型地震解释剖面(剖面位置见图 1)

    Figure  2.  Typical seismic interpretation profiles of the south slope zone of the Laizhouwan Sag

    图  3  莱州湾凹陷南部斜坡带典型剖面构造演化分析

    Figure  3.  Tectonic evolution analysis of typical profiles of the south slope zone of the Laizhouwan Sag

    图  4  KL16-1-2井泥岩声波时差法计算剥蚀厚度

    Figure  4.  Denudation thickness of mudstone in KL16-1-2 well calculated by sound wave time difference method

    图  5  沙四—沙三下亚段沉积时期盆地原型

    Figure  5.  Basin prototype at the sedimentary period in the lower third sub-member and the fourth member of the Shahejie Formation

    图  6  东西部不同位置剥蚀厚度差异(剖面位置见图 5)

    Figure  6.  Denudation thickness difference at different locations in the east and west

    图  7  沙四—沙三下亚段沉积体系展布

    a—沙四段沉积体系展布;b—沙三下亚段沉积体系展布

    Figure  7.  Distribution of sedimentary system in the lower third sub-member and the fourth member of the Shahejie Formation

    图  8  不同沉积体系发育特征(剖面位置见图 5)

    Figure  8.  Development characteristics of different sedimentary systems

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  • 收稿日期:  2017-11-06
  • 修回日期:  2018-04-20
  • 刊出日期:  2018-06-28

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