新疆石油地质 ›› 2023, Vol. 44 ›› Issue (6): 657-666.doi: 10.7657/XJPG20230603

• 油气勘探 • 上一篇    下一篇

基准面旋回控制下的浅水三角洲砂体分散体系特征

赵春晨1(), 刘豪2()   

  1. 1.陕西工业职业技术学院 a.土木工程学院;b.咸阳市数字城市与地理空间大数据技术重点实验室,陕西 咸阳 712000
    2.中国地质大学(北京) 海洋学院,北京 100083
  • 收稿日期:2023-07-29 修回日期:2023-08-24 出版日期:2023-12-01 发布日期:2023-11-29
  • 通讯作者: 刘豪(1974-),男,重庆人,教授,博士,层序地层学,(Tel)13488664388(Email)lhcugb@163.com
  • 作者简介:赵春晨(1987-),男,陕西城固人,高级工程师,博士,层序地层学,(Tel)13279513008(Email)zhaochunchen119@163.com
  • 基金资助:
    陕西工业职业技术学院青年科技创新团队(KCTD2022-01);陕西工业职业技术学院高层次人才科研项目(2020-03);中国地质大学(北京)科研项目(3-4-2013-009)

Characteristics of Sand Body Dispersion System in Shallow-Water Delta Controlled by Base-Level Cycle

ZHAO Chunchen1(), LIU Hao2()   

  1. 1. Shaanxi Polytechnic Institute, a.School of Civil Engineering; b.Xianyang Key Laboratory of Digital City and Geospatial Big Data Technology, Xianyang, Shaanxi 712000, China
    2. School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
  • Received:2023-07-29 Revised:2023-08-24 Online:2023-12-01 Published:2023-11-29

摘要:

松辽盆地浅水三角洲油气藏发育,储集层预测难度大是制约该盆地油气勘探开发的重要因素。秉承地质-地震紧密结合的思想,基于高分辨率地震和高精度层序地层分析,利用地震90°相位转换、正演模拟、地震属性分析等技术,对松辽盆地杏西地区姚家组的层序地层、储集层地质-地球物理响应、砂体分散体系时空演化等方面开展了研究,并探讨了基准面变化对砂体分散体系展布的影响。研究结果表明:杏西地区姚家组可划分为2个中期基准面旋回,识别出3种岩性组合;在地震剖面上,中等厚度砂岩夹薄层泥岩的岩性组合对应强振幅,复合厚互层的岩性组合对应中等—强振幅,薄互层的岩性组合对应弱—中等振幅;基准面上升早期,浅水三角洲砂体分散体系平面上以朵状为主,上升中—晚期,逐渐过渡为退积式树枝状浅水三角洲,基准面下降早期,以加积-微弱进积式树枝状浅水三角洲为主,至下降中—晚期,砂体分散体系以坨状沉积体为主。

关键词: 松辽盆地, 杏西地区, 浅水三角洲, 砂体分散体系, 基准面旋回, 正演模拟, 岩性组合

Abstract:

Shallow-water delta reservoirs are developed in the Songliao basin, where the difficulties in reservoir prediction are restricting oil and gas exploration and development. Adhering to the idea of geology-seismology integration and based on high-resolution seismic survey and high-precision sequence stratigraphy, the Yaojia formation in the Xingxi area of the Songliao basin was investigated with respect to sequence stratigraphy, geophysical responses of reservoirs, and spatio-temporal evolution of sand body dispersion system by using the techniques such as 90° seismic phase conversion, forward modeling, and seismic attribute analysis, and the impact of base-level changes on the distribution of dispersion system was discussed. The results indicate that the Yaojia formation in the Xingxi area can be divided into two mid-term base-level cycles, with three identified lithological combinations. On seismic sections, the lithological combination of moderately-thick sandstones intercalated with thin mudstones corresponds to strong amplitudes; the lithological combination of composite thick interbeds corresponds to medium-strong amplitudes; and the lithological combination of thin interbeds corresponds to weak-medium amplitudes. In plane, the sand body dispersion system in the shallow-water delta primarily exhibited a lobe shape in the early stage of base-level rise, gradually transited into a retrogressive dendritic shallow-water delta in the middle-late stage of base-level rise, existed predominantly as progradational-weakly aggradational dendritic shallow-water deltas in the early stage of base-level fall, and appeared as lump-like deposits in the middle-late stage of base-level fall.

Key words: Songliao basin, Xingxi area, shallow-water delta, sand body dispersion system, base-level cycle, forward modeling, lithologi- cal combination

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