马来西亚马来盆地b组浅层碎屑岩储层沉积相、沉积环境及储层物性

N. Bashiron, S. Johari, A. Sidek, A. Agi, M. H. Ariffin, A. Supee, N. Ridzuan, S. Mahat
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引用次数: 0

摘要

马来西亚Terengganu海上Malay盆地ms油田b组浅层储层进行了勘探开发。对沉积环境、地层背景、岩相、储层几何形状、储层质量和非均质性的不了解是开发这些浅层储层所遇到的一些困难。在本研究中,通过进行储层结构和质量分析,克服了这些挑战。这是通过综合岩心、测井、岩石学和岩石物理分析的解释来实现的,这些分析用于生成沉积模型、描述岩相、以及储层的几何形状、连续性和质量确定。b组岩相类型为层状泥岩(ML)、生物扰动泥岩(MB)、异质泥岩(MH)、异质砂岩(SH)和生物扰动砂岩(SB)。ML岩相和SB岩相的储层质量为中等至良好,SH岩相和MH岩相的储层质量为高至低。该研究为ms油田浅层储层非均质性提供了更好的认识,所得结果也可应用于其他类似浅层储层的表征和建模改进过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sedimentary Facies, Depositional Environment and Reservoir Quality of Group-B Shallow Clastic Reservoir in the Malay Basin, Malaysia
Shallow reservoirs in Group-B of MS-field in Malay Basin, Terengganu's offshore, Malaysia were explored for development. Poor understanding of depositional settings, stratigraphic context, lithofacies, reservoir geometry, reservoir quality, and heterogeneity are some of the difficulties encountered in developing these shallow reservoirs. In this study, these challenges were circumvented by performing reservoir architecture and quality analysis. This was achieved by integrating the interpretation from the cores, well logs, petrographic and petrophysical analyses for depositional model generation, lithofacies description, as well as reservoir geometry, continuity, and quality determination. Five lithofacies were identified in Group-B, namely: laminated mudstone (ML), bioturbated mudstone (MB), heterolithic mud dominated (MH), heterolithic sand dominated (SH), and bioturbated sandstone (SB). The sediments encountered in ML and SB lithofacies consist of moderate to good reservoir quality, while for SH and MH, they ranged from high to low quality. This study provides a better insight to the shallow reservoir heterogeneity in MS-field and the results obtained could also be applied to the other similar shallow reservoirs for characterization and modelling improvement processes.
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