地学前缘 ›› 2015, Vol. 22 ›› Issue (1): 386-396.DOI: 10.13745/j.esf.2015.01.033

• 非主题来稿选登 • 上一篇    

利用地层切片研究陆相湖盆深水滑塌浊积扇沉积特征

董艳蕾,朱筱敏,耿晓洁,汪海,王茂文, 姜青梅,杜远宗   

  1. 1. 中国石油大学 地球科学学院, 北京 102249
    2. 中国石油大学 油气资源与探测国家重点实验室, 北京 102249
    3. 中国地质大学(北京) 能源学院, 北京 100083
    4. 中原油田天然气产销厂, 河南 濮阳 457000
  • 收稿日期:2014-01-02 修回日期:2014-03-27 出版日期:2015-01-15 发布日期:2015-01-15
  • 作者简介:董艳蕾(1972—),女,博士,讲师,主要从事层序地层学、地震沉积学及地震地貌学方面的研究工作。E-mail:yanleidong@163.com
  • 基金资助:

    国家自然科学基金项目“陆相断陷湖盆深水浊积扇定量地震地貌学研究”(41202078);中国石油大学(北京)科研基金资助项目“陆相盆地不同类型砂体地震沉积学模式研究”(KYJJ2012-01-31)

Using the stratal slice to study the depositional characteristics of deep-water slumped turbidite fans in continental lake basin

  • Received:2014-01-02 Revised:2014-03-27 Online:2015-01-15 Published:2015-01-15

摘要:

以泌阳凹陷核三段上部层序为例,首先建立高分辨层序格架,然后以地震沉积学思想为指导,利用地层切片技术,制作了展现沉积微相分布和沉积演化过程的切片数据体。通过岩心、录井、测井等资料的标定,对典型地层切片进行了精细解释。研究认为,泌阳凹陷深凹区主要接受东北部、东南部和西南部三大剥蚀区的陆源碎屑供给,对应发育东北部侯庄辫状河三角洲、东南部梨树凹近岸水下扇和西南部杨桥近岸水下扇沉积体系,而深凹区内多发育滑塌浊积扇沉积。地震剖面显示透镜状地震反射与前积地震反射共生,通过对连续地层切片的比较研究,刻画出辫状河三角洲与滑塌浊积扇的成因关系。最终预测了各类沉积相在时空上的展布和演变,为该凹陷寻找滑塌浊积扇等隐蔽油气藏提供了较为可靠的依据,研究成果在2010年8月完钻的安深1井得到了证实。

关键词: 地层切片, 地震沉积学, 滑塌浊积扇, 核三段, 泌阳凹陷

Abstract:

The upper He-3 sequence of the Biyang Sag is used in this paper as an example to illustrate the workflow of Seismic Sedimentology. On the basis of subtle sequence framework, a stratal slice cube was made which displayed the distribution of sedimentary microfacies, and the analysis of the cube enabled the interpretation of the evolutionary history. Through the comprehensive analysis of core, lithology and well-logging, the sandbodies of the typical slices were interpreted elaborately, and some conclusions were drawn as follows. There exist three denuded areas in the north-east, south-east and south-west, respectively, which provided the terrigenous clasts to the deep depression of the Biyang Sag, and where developed correspondingly the three sedimentary formations, i.e., the Houzhuang braided delta in the north-east, the Lishuwa nearshore subaqueous fan in the south-east and the Yangqiao nearshore subaqueous fan in the south-west. In the deep depression, slump turbidite fans were developed. The progradational configuration of braided delta front always associated with the lenticular reflection in strike direction, which showed the process of the sand bodies sliding from delta front into semideep to deep lacus and being wrapped by mudstone. Finally, the paper predicts the distribution of sedimentary facies and provides the reliable evidence of exploration of subtle traps such as slump turbidite fans. The result was verified by Well Anshen 1.

Key words: stratal slice, seismic sedimentology, slump turbidite fan, He-3 Formation, Biyang Sag

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