›› 2014, Vol. 35 ›› Issue (4): 1-1.

• 论文 •    

基于地震沉积学的高频层序解释方法 ——以莺歌海盆地A区为例

陈志宏1,2,应明雄2,陈殿远2   

  1. (1.中国地质大学 资源学院,武汉 430074;2.中国海油 湛江分公司,广东 湛江 524057)
  • 出版日期:2019-01-01 发布日期:1905-07-13

HighFrequency Sequence Unit Interpretation Method Based on Seismic SedimentologyAn example from DistrictA in Yinggehai basin

CHEN Zhihong1,2, YING Mingxiong2, CHEN Dianyuan2   

  1. (1.School of Resource, China University of Geosciences, Wuhan, Hubei 430074, China; 2. Zhanjiang Branch, CNOOC, Zhanjiang,Guangdong 524057, China)
  • Online:2019-01-01 Published:1905-07-13

摘要: 传统的高频层序解释是在测井资料约束下进行地震层位的解释追踪对比,该方法并不适用于少井或无井及低分辨率地震资料的地区。通过莺歌海盆地A地区典型实例分析,介绍了一种运用地震沉积学进行高频层序解释的新方法,即在三级层序地层格架控制下,运用地震沉积学方法,将识别出的高分辨率水平沉积单元分布规律(平面图)与垂向高频层序界面的解释有机结合,从而提高高频层序单元划分精度。该方法包括3个步骤:地震数据体向岩性数据体的转换;运用地震地貌学方法初步确定高频层序界面位置;运用分频剖面技术约束和调整高频层序界面。该方法改变了常规地震解释顺序,在高频层序地层学研究中将垂向上地震剖面的高频单元分析与横向上高分辨率地震引起的地貌特征信息有机结合,使得高频层序界面的追踪以及三维空间成像变得更加快捷、准确。

Abstract: The traditional high?frequency sequence analysis as the most commonly used approach focuses on the interpretation and correlation of seismic markers constrained by well logging data, but it could not be applied in the area with few well data and low?resolution seismic profiles. In this paper, a new approach on high?frequence sequence analysis based on seismic sedimentology is presented, and a new seismic?sedimentological approach for mapping high?frequency sequence by a case study is introduced. First, we used seismic sedimentology to investigate high?resolution horizontal (plan view) depositional elements is the third?order sequence stratigraphic framework; then, we examined their high?frequency sequence?stratigraphic context in vertical and 3?D view. The new approach included three steps: 1)converting a 3?D seismic volume into a lithology volume; 2)defining the high?frequency sequence boundaries by using seismic geomorphology; 3)adjusting the high?frequency sequence stratigraphic studies under the control of frequency decomposing profile. The new interpretation procedure shifts the emphasis of high?frequence sequence stratigraphic studies from interpreting vertical seismic profiles to analyzing more horizontal, high ?resolution and seismic ? geomorphologic information, which allows the tracing of high ?frequence sequence stratigraphic boundaries and the 3?D imaging to be realized more quickly and accurately

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