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Identification of seismic facies and its sedimentary facies prediction in DD block

机译:DD区块地震相识别及沉积相预测

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The DD block is a new exploration area with relative complex structure. At present, due to the lack of any well revealing the target formation (XL formation), previous related studies on its sedimentary facies were mainly based on regional geologic understanding, so it can''t provide both available sedimentary facies belt and favorable reservoir area for further exploration and development activities. In this paper, under the guideline of the theory of sequence stratigraphy, based on the only more than 400 kilometers 2-D seismic data (with survey grid of 2×3∼3×4 km) in our study area, together with outcrop data, regional depositional setting and previous studies, the authors analyzed the reflection signature and identified its lithology within the XL formation on each seismic profile, then compiled lateral comprehensive vector analysis in profile and plane, after that, we divided seismic facies belts and converted them into sedimentary facies with the help of geological understanding. Finally, the plane distribution of some potential favorable sedimentary facies for reservoir development within the XL formation is outlined. Due to its high-quality seismic data with distinct reflection characteristic, the prediction results can provide some useful information for oil and gas exploration in this area.
机译:DD区块是一个结构相对复杂的新勘探区。目前,由于缺乏揭示目标形成(XL形成)的井,以前有关其沉积相的相关研究主要基于区域地质认识,因此无法同时提供可用的沉积相带和有利的储层面积。进行进一步的勘探和开发活动。本文在层序地层学理论的指导下,以研究区仅400多公里的二维地震数据(调查网格为2×3〜3×4 km)和露头数据为基础,区域沉积环境和以前的研究,作者分析了反射特征,并在每个地震剖面上的XL地层中确定了其岩性,然后在剖面和平面上进行了横向综合矢量分析,之后,我们划分了地震相带并将其转换为地质认识的帮助下的沉积相。最后,概述了XL地层中一些潜在的有利沉积相的平面分布,这些沉积相对于储层发育具有重要意义。由于其高质量的地震数据具有独特的反射特征,因此预测结果可以为该地区的油气勘探提供一些有用的信息。

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