Evaluation of Abu Madi Formation in Baltim North & East gas fields, Egypt, using seismic interpretation and well log analysis

H. H. E. Kadi, S. Shebl, M. Ghorab, A. Azab, M. Salama
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引用次数: 6

Abstract

ABSTRACT Abu Madi Formation is a gas fertile rock unit in Nile Delta basin and the main gas production rocks in Baltim fields which located in the Mediterranean sea, north of Baltim city, Egypt. This rock unit in the study area contains two gas productive sand zones; these are zone III main and zone III lower. The lithologic components of Abu Madi Formation that defined from the dia-porosity (density–neutron) cross-plot and the tri-porosity (RHOMAA–DTMAA) cross-plot, showing that, Abu Madi Formation consists mainly of sandstone, shale, shaly sandstone in some parts and calcareous material. The resultant petrophysical parameter values, revealed that, both zone III main and zone III lower in the area under investigation show potential in their petrophysical characteristics, as a fertile gas reservoir. Zone III lower shows the most advanced petrophysical characterisation as a desired reservoir, with lower value of shale volume of 4%, good effective porosity of 17% and higher value of hydrocarbon saturation of 70%. Finally, these reservoirs are bounded by two normal faults with remarkable displacement. The first fault located at south, strike E - W and dips toward the North, the other fault located north, trending NE- SW and dips to the north.
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利用地震解释和测井分析评价埃及Baltim东北气田Abu Madi组
Abu Madi组位于埃及巴尔提姆市以北的地中海沿岸,是尼罗河三角洲盆地的富气岩单元,也是巴尔提姆气田的主要产气岩。研究区该岩单元含2个产气砂带;这些是第三区主要和第三区较低。通过介质-孔隙度(密度-中子)交叉图和三孔隙度(RHOMAA-DTMAA)交叉图确定了Abu Madi组的岩性成分,表明Abu Madi组主要由砂岩、页岩、部分泥质砂岩和钙质物质组成。岩石物性参数值表明,研究区主III带和下III带均具有丰富的储层岩石物性特征。下III区岩石物性特征最先进,页岩体积值较低,为4%,有效孔隙度较好,为17%,烃饱和度较高,为70%,为理想储层。最后,这些储层被两条位移显著的正断层所包围。第一个断层位于南部,走向东西向,向北倾;另一个断层位于北部,走向NE- SW,向北倾。
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