地震地貌学作为储层表征的工具:以泰国湾pattani盆地moragot油田为例

S. Hossain
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引用次数: 4

摘要

Pattani盆地拥有泰国湾最多的油气生产油田。早-中中新世河道和河岸砂是该盆地的主要储层。由于这些砂的垂直和水平分布非常有限,因此基于常规地震解释并不总是容易预测这些砂的几何形状和分布。本研究旨在利用RMS振幅分析、光谱分解、相似度和倾角控制相似度等先进成像技术,研究不同地层层段的地震地貌,预测砂体分布。为此,学习时间分为三个时间段。在第一阶段,RMS和semsimilarity成功地识别了与河道带相关的砂体和泥质河道。另一方面,通过使用光谱分解和倾角导向相似体积,可以更有效地成像较深的地层水平(第2期和第3期)。这些属性体的层位切片显示了砂泥通道在不同层位上的分布。河道带的宽度从200米到3公里不等。这些水道带呈北南向和北西-东南向。然后,通过测井分析和对比验证了这三(3)个时期的地震地貌分析结果。第3期水平片的宽水道带对应于测井记录的堆积水道砂体。而在测井2期,窄水道带对应薄砂单元。在这段时间内还发现了煤的广泛赋存。1期测井资料显示,水平片曲流带发育良好,呈精细向上演替。在地层切片中发现的泥质河道可能起到屏障作用,将储层分隔开来。本研究提出的砂体分布预测工作流程有助于降低勘探风险,并有助于规划充填开发井。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SEISMIC GEOMORPHOLOGY AS A TOOL FOR RESERVOIR CHARACTERIZATION: A CASE STUDY FROM MORAGOT FIELD OF PATTANI BASIN, GULF OF THAILAND
Pattani Basin hosts the greatest number of hydrocarbons producing fields in the Gulf of Thailand. Early to Middle Miocene fluvial channel and overbank sands are the main reservoirs in this basin. Due to their nature of very limited vertical and horizontal distribution it is not always easy to predict the geometry and distribution of these sands based on the conventional seismic interpretation. This study aims to study seismic geomorphology at different stratigraphic intervals to predict sand distribution by applying advanced imaging techniques such as RMS amplitude analysis, spectral decomposition, semblance and dip steered similarity. For this purpose, the study interval is divided into three periods. In period 1, RMS and semblance successfully identified sand bodies and mud filled channels associated with channel belts. On the other hand, deeper stratigraphic levels (period 2 & 3) can be imaged more effectively by using spectral decomposition and dip steered similarity volumes. Horizon slices from these attribute volumes show the distribution of sands and mud filled channels at different stratigraphic level. The width of channel belts varies from 200 m to 3 km. These channel belts are N-S and NW-SE oriented. The findings from seismic geomorphology analysis in these three (3) periods were then validated by well log analysis and correlation. Broad channel belts in horizon slices in period 3 correspond to stacked channel sands in well log. Whereas narrow channel belts correspond to thin sand units in well log in period 2. Widespread occurrence of coals has also been noticed in this interval. Very well-developed meander belts in horizon slices are transpired as fining upward succession in well logs in period 1. Mud filled channels identified in the horizon slices might act as a barrier and compartmentalize the reservoir. The proposed workflow of predicting sand distribution in this study might help to reduce exploration risk as well as in planning infill development wells.
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