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Understanding the hydrocarbon prospect of Buzdar block, Southern Indus basin, Pakistan, by using 2-D seismic data: A case study

机译:了解Buzdar块的碳氢化合物前景,通过使用2-D地震数据,巴基斯坦(巴基斯坦)南部南部盆地盆地的前景:一个案例研究

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The sub-surface structural analysis to understand the geology and tectonics of an area is always useful to locate the hydrocarbon resources. Oil and gas based energy supplies have become a vital source for Pakistan, which is passing through an era of severe energy crisis. The study area, Buzdar block, in the southern Indus Basin is tectonically an extensional regime and is expected to have a huge hydrocarbon potential. In this study, we did the interpretation of the migrated seismic lines of the 872-SGR-527, 872-SGR-529, 872-SGR-531, 872-SGR-532 of Buzdar block, District TandoAllahyar, Sindh. The lines 872-SGR-529, 872-SGR-531, 872-SGR-532 were oriented Wa??E whereas the line 872-SGR-527 was oriented NWa??SE. The obtained data was analysed and three reflectors were marked named top Khadro Formation, top lower Goru formation and top Chiltan limestone (probable). Through this study faults have been also marked on seismic lines which are normal faults by nature; collectively form horsts and grabens which is the evidence of effect of extensional tectonics in the area. Time contour maps were also generated. After that, time was converted into depth with the help of well velocity from VSP data for lower Goru formation and average velocity for Chiltan limestone (probable) from regression analysis. Finally, depth contour maps were generated which helped to know the basic mechanism of tectonic movement in the area. On the basis of present analysis we propose that a well may be drilled at Lower Goru formation near fault F1 on western side at a depth of 1370 meters and at 1290 meters near fault F4 on eastern side.
机译:亚表面结构分析以了解区域的地质和构造始终有用的是定位碳氢化合物资源。石油和天然气的能源供应已成为巴基斯坦的重要来源,它正在通过严重的能源危机时代。研究区Buzdar块,在南部的南部盆地是一个扩张的制度,预计将具有巨大的碳氢化合物潜力。在这项研究中,我们对872-SGR-527,872-SGR-529,872-SGR-531,872-SGR-531,872-SGR-532,SINDH,SINDH区的872-SGR-531,872-SGR-532的迁移地震线进行了解释。线872-sgr-529,872-sgr-531,872-sgr-532取向waΔωe,而872-sgr-527是定向的nwaα。分析了所获得的数据,并标记了三个反射器,称为顶部Khadro形成,下部Goru形成和顶部Chiltan石灰石(可能)。通过这项研究,缺陷也标志着自然界正常的地震线;集体形成Horsts和Grabens,这是该地区延伸构造的影响的证据。还生成了时间轮廓图。之后,在从VSP数据的良好速度下,从VSP数据的良好速度转换为深度,从而从回归分析到沉淀物石灰石(可能)的平均速度。最后,产生了深度等值图,这有助于了解该地区的构造运动的基本机制。在现有分析的基础上,我们提出了在西侧的较低的Goru形成附近的较低的Goru地层钻井,深度为1370米,在东部靠近故障F4附近1290米。

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