Structural Styles and their Suitability for Hydrocarbon in Eastern Sindh Monocline, Lower Indus Basin, Pakistan

Mujeeb Rehman Khaskheli, Muhammad Hassan Agheem, Manzoor Ali Panhwar, Ulfat Akram, Jabir Nazir
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Abstract

The present study is aimed to recognize the structural styles of hydrocarbon exploration and petrophysical properties of the LGF. The 2-D seismic and well log data set is composed of three seismic lines and well log data of Chak 66–1. Five horizons have been marked with the help of well to seismic tie namely tops of Ranikot, Parh, upper Goru, lower Goru, basal and top massive sands, and out of which basal and massive sands are the objective focus of the present study. Based on seismic data, the study area is characterized by normal faults showing NW–SE dipping trend. Horst and graben structural features are prominent on the seismic lines, which indicated the extensional tectonic regime. Time–depth contour maps and 3D surfaces of objective horizons depict their actual spatial distribution in this area. Wireline logging analysis revealed the physical properties of both basal and massive grains of sand, as 17% effective porosity, 25% average volume of shale (Vsh), 40% water and 60% hydrocarbon saturations for basal sands, Whereas, 16% effective porosity, 35% Vsh, 30% water and 70% hydrocarbon saturations are interpreted for massive sands. Cross–plots of Nphi–Dt and Dt–Rhob also identified that both areas of sand are clean, gas–saturated and have the potential to produce hydrocarbons.
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巴基斯坦下印度河盆地信德单斜东部构造样式及其油气适宜性
本研究旨在识别下第三系油气勘探的构造样式和岩石物理性质。二维地震测井资料集由察66-1的三条地震线和测井资料组成。通过井震测井,确定了Ranikot顶部、Parh顶部、上Goru顶部、下Goru顶部、基底和顶部块状砂岩五个层位,其中基底和块状砂岩是本研究的客观重点。根据地震资料,研究区为北西-东倾正断层。地震线上具有明显的地堑和地垒构造特征,表明其为伸展构造。时深等高线图和物镜视界的三维曲面描绘了它们在该区域的实际空间分布。电缆测井分析显示,基岩和块状砂岩的物理性质为有效孔隙度为17%,平均页岩体积(Vsh)为25%,含水饱和度为40%,含油饱和度为60%,而块状砂岩的有效孔隙度为16%,平均页岩体积(Vsh)为35%,含水饱和度为30%,含油饱和度为70%。Nphi-Dt和Dt-Rhob的交叉图也表明,这两个砂区都是清洁的,天然气饱和的,具有生产碳氢化合物的潜力。
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