新疆石油地质 ›› 2020, Vol. 41 ›› Issue (1): 108-113.doi: 10.7657/XJPG20200113

• 应用技术 • 上一篇    下一篇

准噶尔盆地南缘四棵树地区中浅层砾岩层识别刻画

范旭, 刘宜文, 郑鸿明, 马俊彦, 尹丽丽   

  1. 中国石油 新疆油田分公司 勘探开发研究院 地球物理研究所,乌鲁木齐 830013
  • 收稿日期:2019-10-29 修回日期:2019-11-11 出版日期:2020-02-01 发布日期:2020-03-31
  • 作者简介:范旭(1968-),男,安徽庐江人,高级工程师,地震资料处理,(Tel)13999930900(E-mail)fanx@petrochina.com.cn
  • 基金资助:
    国家油气重大专项(2016ZX05003-005)

Identification and Characterization of Middle-Shallow Conglomerates of Sikeshu Area in the Southern Margin of Junggar Basin

FAN Xu, LIU Yiwen, ZHENG Hongming, MA Junyan, YIN Lili   

  1. Geophysics Institute, Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Urumqi, Xinjiang 830013, China
  • Received:2019-10-29 Revised:2019-11-11 Online:2020-02-01 Published:2020-03-31

摘要:

准噶尔盆地南缘中、下组合构造普遍位于中浅层砾岩层之下,砾岩层具有横向展布范围广且不规则、纵横向速度变化大等特点,严重制约中、下组合目标的精细落实。因此,搞清砾岩层结构及分布特征,对下伏构造形态和高点位置的准确落实尤为重要。结合微测井、钻井、测井资料以及地震剖面对准噶尔盆地南缘四棵树地区中浅层砾岩层结构特征进行分析,对低速和高速砾岩层的顶底界面进行识别刻画,并分区、分段建立了砾岩层时深关系曲线,用于指导深度域下组合构造成图和叠前深度偏移中浅层速度模型的建立。实例应用证明,南缘四棵树地区中浅层砾岩层识别刻画对准确落实构造目标,提高地震剖面成像品质至关重要,同样也可以在准噶尔盆地南缘其他类似地区进行推广应用。

关键词: 准噶尔盆地, 四棵树地区, 中浅层, 低速砾岩层, 高速砾岩层, 识别刻画, 时深关系, 速度建模

Abstract:

The middle-lower assemblage structure in the southern margin of Junggar basin is generally located below the middle-shallow gravel belt, and the conglomerates are characterized by wide and irregular lateral distribution and large variations of vertical velocity, which seriously restrict the fine identification of the targets in the middle-lower assemblage. Therefore, it is very important to figure out the structure and distribution of the gravel belt for accurately identifying the configuration and high point position of the underlying structure. Combining micro-logging and drilling data with seismic sections, the paper analyzes the structural characteristics of middlle-shallow conglomerates, describes the top and bottom interfaces of low-speed and high-speed conglomerate intervals of the Sikeshu area in the southern margin of Junggar basin, and establishes time-depth curves by districts and sections, which can be used to guide the accurate depth-domain mapping of composite structures and the velocity model building of the middle and shallow layers for prestack depth migration. The application result shows that the identification and characterization of the middle-shallow conglomerate of the Sikeshu area in the southern margin of Junggar basin is of great help for the accurate determination of the structural objectives and the imaging quality improvement of the seismic sections, which can also be applied in other similar areas in the southern margin of Junggar basin.

Key words: Junggar basin, Sikeshu area, middle-shallow layer, low-speed conglomerate interval, high-speed conglomerate interval, identi- fication and description, time-depth relation, velocity modelling

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