中国石油勘探 ›› 2019, Vol. 24 ›› Issue (6): 721-729.DOI: 10.3969/j.issn.1672-7703.2019.06.004

• 勘探案例 • 上一篇    下一篇

南苏丹迈卢特盆地北部凹陷古近系Yabus 组浅水三角洲沉积特征

王林1 ,史卜庆1 ,史忠生2 ,郑凤云3 ,马洪1   

  1. 1 中国石油国际勘探开发有限公司;2 中国石油勘探开发研究院西北分院;3 中国石油勘探开发研究院
  • 出版日期:2019-11-15 发布日期:2019-11-15
  • 基金资助:
    国家科技重大专项“海外重点探区目标评价与未来领域选区选带研究”(2016ZX05029005)。

Sedimentary characteristics of Paleogene Yabus Formation in shallow-water delta in the northern sag of the Melut Basin, South Sudan

Wang Lin1, Shi Buqing1,Shi Zhongsheng2,Zheng Fengyun3,Ma Hong1   

  1. 1 China National Oil and Gas Exploration and Development Co., Ltd.; 2 Northwest Branch, PetroChina Research Institute of Petroleum Exploration & Development; 3 PetroChina Research Institute of Petroleum Exploration & Development
  • Online:2019-11-15 Published:2019-11-15
  • Supported by:
     

摘要: 以南苏丹断陷湖盆迈卢特盆地为例,通过区域地质、岩心、测井、粒度及地震相等资料的分析研究,认 为北部凹陷弱裂陷期形成的古近系Yabus 组发育浅水三角洲沉积。受盆地裂陷活动与湖平面变化影响,Yabus 组上 段和下段具有不同的浅水三角洲沉积特征。Yabus 组下段沉积时期,盆地构造活动弱,湖盆水体浅,以发育广泛分布 的浅水三角洲平原分流河道为特征。Yabus 组上段沉积时期,盆地裂陷活动增强,湖盆水体缓慢加深,形成了广泛分 布的浅水三角洲前缘沉积及局部的滨浅湖沉积,水下分流河道、河口坝等砂体在断层配合下可形成构造—岩性圈闭, 研究成果对迈卢特盆地北部凹陷的成熟探区滚动挖潜与精细勘探具有重要意义。

 

关键词: 迈卢特盆地, 古近系, Yabus 组, 浅水三角洲, 沉积特征

Abstract: Taking the north sag in the Melut Basin in South Sudan as a case, researches were carried out based on regional geology, cores, logging data, grain sizes and seismic facies, which showed that the Paleogene Yabus Formation is a shallow-water delta facies developed in the weak rifting period of the northern sag. In?uenced by rifting activities and lake water level, the upper and lower members of the Yabus Formation have different sedimentary characteristics of shallow-water deltas. During the sedimentary period of the lower member, basin tectonic activities were weak, and the lake water was shallow, so distributary channels of the shallow-water delta plain were widely developed. During the sedimentary period of the upper member, rifting activities were intensive, and the lake water became deep, so there developed widely distributed shallow-water delta frontal sediments and local coastal shallow lake sediments. The underwater distributary channels, distributary mouth bars and other sand bodies may form structural-lithologic traps controlled by faults. The research results are of great signi?cance for continuously estimating the potential and ?nely exploring in the mature exploration areas in the northern sag of the Melut Basin.

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