第9届中东地球科学会议,2010.科威特Minagish油田鲕粒储层高分辨率地震模拟研究。

A. Ebaid
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引用次数: 0

摘要

Minagish油田有几个油藏,石油主要聚集在下白垩统Minagish鲕粒岩(MMO)中段。这一巨大的碳酸盐岩油气藏发现于1959年,占该油田石油产量的90%以上。随着储层压力开始下降,需要在结构侧翼注水以支撑储层压力并提高产油量。基于测井、岩心和旧三维地震资料的层序地层分析将储层划分为13个地质层,具有多期鲕滩发育。Minagish Oolite油藏在油柱下方有50至120英尺厚的焦油垫。它存在于许多侧翼井中,但不是全部。它发生在不同的深度,在9700英尺到9935英尺的TVDSS之间,并且在油田的南部更深。水被注入沥青垫层的上下两层,以支持水库对顶部的压力。注水井MN“A”井的井监测数据解释表明,沥青垫层以下的层的注入能力与上面的层相比非常低。附近的生产井MN“B”显示上层有水突破,而下层不受水的影响。下部鲕粒沉积物可能具有中等进积的斜地形叠加模式,旧的常规三维地震资料对其成像较弱。井间淹水事件的定义存在一定的不确定性。2006年,为了改善储层特征,进行了高分辨率三维地震勘探。在Minagish构造的东部发现了渐进式倾斜斜形几何形状,这使我们更好地定义了该地区的储层结构。这对Minagish鲕粒储层建模有直接影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impact of high-resolution seismic from reservoir modeling Minagish Oolite reservoir, Minagish Field, Kuwait. 9th Middle East Geosciences Conference, GEO 2010.
The Minagish Field has several reservoirs with oil accumulated primarily in the Lower Cretaceous middle member of the Minagish Oolite rocks (MMO). This giant carbonate hydrocarbon accumulation was discovered in 1959 and accounts for over 90% of oil production in the field. As the reservoir pressure started to decline, there was a need for water injection on the flanks of the structure to support the reservoir pressure and to increase the oil production. The sequence-stratigraphic analysis based on well logs, cores and the old 3-D seismic subdivided the reservoir into 13 geological layers with multiple phases of ooid shoal development. The Minagish Oolite reservoir has a 50 to 120 feet thick tar mat underlying the oil column. It is present in many, but not all, flank wells. It occurs at differing depths, between 9,700 ft and 9,935 ft TVDSS, and is deeper to the south of the field. The water has been injected in the layers above and below the tar mat in order to support the reservoir pressure on the crest. The well surveillance data interpretation of the injector Well MN “A” shows that layers below tar mat have very low injectivity compared with the layers above. The nearby producing Well MN “B” shows a water breakthrough in the upper layers whereas the lower layers are not affected by water. The lower oolite sediments possibly have a moderately progradational clinoforms stacking pattern which are weakly imaged by the old conventional 3-D seismic data. There is some uncertainty in the definition of flooding events between wells. In 2006, a high-resolution 3-D seismic survey was acquired to improve reservoir characterization. Progradational dipping clinoforms geometries are detected to the east of Minagish structure which led us to better definition of the reservoir architecture at this particular area in the field. This has a direct impact on Minagish Oolite reservoir modeling.
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