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Evaluation of Reservoir Characteristics of Well Kot-Sarang-2, Potwar Plateau, Pakistan Using Geophysical Logs

机译:利用地球物理测井评价巴基斯坦Potwar高原Kot-Sarang-2井的储层特征

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Present study deals with reservoir characterization of Kot-Sarang-2 well, located in central part of Potwarplateau of Upper Indus Basin, District Chakwal. The geological structure of the Potwar Basin is the product of theTertiary Himalayan orogeny, which resulted in the formation of complex fold and thrust belt in this region. In thepresent work, an attempt has been made to delineate zones having fair shows of hydrocarbons accumulation. Inaddition to this, estimation of reservoir properties and formation evaluation using wireline logs is also the foremostobjective of this study. Based on the wireline logging results, three zones have been marked. Paleocene LockhartLimestone (3967m to 4045m), Permian Wargal Limestone (4160m to 4245m) and Permian Amb Formation (4246m to4285m) are possible reservoirs encountered. Physical properties i.e. total porosity (豻), effective porosity (谽),resistivity of water (Rw), saturation of water (Sw) and saturation of hydrocarbons (Sh) are calculated. For the calculationof saturation of water (Sw) both Archie抯 equation (Swa) and Indonesian equation (Swi) are applied. Results show thatAmb and Wargal formations are showing fair to good saturation of Hydrocarbons (Sh) i.e.73% and 88% respectively,but this is due to high resistivity values of these formations and porosity log also giving very low values. Effectiveporosity for zones Lockhart, Wargal and Amb are 2.56%, 3.5% and 1.32% respectively. Based on these results it isinferred that these formations have low potential for an economically feasible production of hydrocarbons.
机译:目前的研究是针对位于Chakwal地区上印度河盆地Potwarplateau中部的Kot-Sarang-2井的储层特征。 Potwar盆地的地质结构是喜马拉雅第三纪造山作用的产物,导致该地区形成了复杂的褶皱和逆冲带。在目前的工作中,已经试图划定具有油气聚集的明显迹象的区域。除此之外,使用电缆测井评估储层性质和评价地层也是本研究的首要目标。根据电缆测井结果,已标记了三个区域。古新世洛克哈特石灰岩(3967m至4045m),二叠纪沃加尔石灰岩(4160m至4245m)和二叠纪安布组(4246m至4285m)是可能遇到的储层。计算出物理性质,即总孔隙率(豻),有效孔隙率(谽),水的电阻率(Rw),水的饱和度(Sw)和烃的饱和度(Sh)。为了计算水的饱和度(Sw),应用了Archie抯方程(Swa)和印度尼西亚方程(Swi)。结果表明,Amb和Wargal地层的烃饱和度(Sh)分别达到中等至良好,即分别为73%和88%,但这是由于这些地层的电阻率值很高,而孔隙率测井值也很低。洛克哈特,瓦尔加尔和安布地区的有效孔隙率分别为2.56%,3.5%和1.32%。根据这些结果,可以推断这些地层在经济上可行的烃生产中潜力低。

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