层序地层学对储层表征和构型的控制:以埃及迈西尼亚阿布马迪切谷充填体为例

M. Abdel-Fattah, R. Slatt
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引用次数: 44

摘要

了解断陷谷层序地层构型是了解相对海平面变化对储层表征和构型影响的关键一步。根据地震和钻孔资料,建立了晚墨西尼亚期Abu Madi组切谷地层的层序地层格架。砂体分布分析表明,埃及尼罗河三角洲巴尔提姆油田Abu Madi组河道砂岩在空间和地层位置上不是随机分布的,而是可预测的。在层序地层格架中阐明阿布马迪切谷充填体的砂岩分布,有助于更好地了解其埋藏时期的特征和结构。Abu Madi组地层由两个层序组成,其地层结构最为复杂;它们的沉积物构成了一个复杂的切割山谷填充物。较低的层序(SQ1)由一个较厚的切割山谷填充组成,由一个低水位体系域(LST1)和一个海侵体系域(TST1)和一个高水位体系域(HST1)覆盖。上层序(SQ2)含河道充填,可解释为具有薄砂岩河道沉积的LST2。在此之上,受潮汐影响的河道充填砂岩及相关地层圈定了TST2的基底,并被HST2覆盖。埃及Baltim油田Abu Madi组气藏(现今深度~ 3552 m)由河流低洼体系域(LST)砂岩沉积在一个切割的山谷中。LST砂岩具有较大的孔隙度范围(15 ~ 28%)和渗透率范围(1 ~ 5080mD),反映了沉积相和成岩控制作用。研究结果表明,层序地层分布对切谷沉积储层特征和构型的影响具有约束和评价的价值,从而对此类环境下油气勘探中的储层质量演化具有重要影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sequence stratigraphic controls on reservoir characterization and architecture: case study of the Messinian Abu Madi incised-valley fill, Egypt
Understanding sequence stratigraphy architecture in the incised-valley is a crucial step to understanding the effect of relative sea level changes on reservoir characterization and architecture. This paper presents a sequence stratigraphic framework of the incised-valley strata within the late Messinian Abu Madi Formation based on seismic and borehole data. Analysis of sand-body distribution reveals that fluvial channel sandstones in the Abu Madi Formation in the Baltim Fields, offshore Nile Delta, Egypt, are not randomly distributed but are predictable in their spatial and stratigraphic position. Elucidation of the distribution of sandstones in the Abu Madi incised-valley fill within a sequence stratigraphic framework allows a better understanding of their characterization and architecture during burial.Strata of the Abu Madi Formation are interpreted to comprise two sequences, which are the most complex stratigraphically; their deposits comprise a complex incised valley fill. The lower sequence (SQ1) consists of a thick incised valley-fill of a Lowstand Systems Tract (LST1)) overlain by a Transgressive Systems Tract (TST1) and Highstand Systems Tract (HST1). The upper sequence (SQ2) contains channel-fill and is interpreted as a LST2 which has a thin sandstone channel deposits. Above this, channel-fill sandstone and related strata with tidal influence delineates the base of TST2, which is overlain by a HST2. Gas reservoirs of the Abu Madi Formation (present-day depth ∼3552 m), the Baltim Fields, Egypt, consist of fluvial lowstand systems tract (LST) sandstones deposited in an incised valley. LST sandstones have a wide range of porosity (15 to 28%) and permeability (1 to 5080mD), which reflect both depositional facies and diagenetic controls.This work demonstrates the value of constraining and evaluating the impact of sequence stratigraphic distribution on reservoir characterization and architecture in incised-valley deposits, and thus has an important impact on reservoir quality evolution in hydrocarbon exploration in such settings.
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Central European Journal of Geosciences
Central European Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
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