首页> 外文期刊>Journal of Petroleum Exploration and Production Technology >Analysis of subsurface structural trend and stratigraphic architecture using 2D seismic data: a case study from Bannu Basin, Pakistan
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Analysis of subsurface structural trend and stratigraphic architecture using 2D seismic data: a case study from Bannu Basin, Pakistan

机译:使用2D地震数据对地下结构趋势和地层架构分析 - 以巴基斯坦禁区盆地的一个案例研究

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The present study is focused on the subsurface geology of Bannu Basin, a part of western Indus foreland Pakistan. For this purpose, some regional seismic profiles and deep exploratory wells data have been used in integration.A total of ten mappabale seismic reflection events have been identifed which are representative of specific geological units. In general, based on the seismic the formation trends, the horizons are dipping in the northwest direction of the study area. The area generally deepens toward the northwest due to sediments load toward the northwest. The seismic profile MWI-83 shows a unique faults bounded anticlinal structure that has also been mapped on the two-dimmensional contour maps. This could be regarded as potential hydrocarbon entrapment. The regional seismic profiles are contoured for the entire grid in both time and depth domain to obtain the clearer image of the subsurface individual stratigraphic units. The 2D contour maps for Lower Permian aged Warcha Sandstone, Middle Triassic aged Tredian Formation and Early Jurrasic aged Datta Formation have been prepared using gridded TWT of the seismic profiles. The time and depth contour maps of the Datta Formation and Tredian Formation show a four way clouser oriented in the southeast dierction. The area of the closure was computed which is 24 Sq km approximately. Furthermore, the formation tops of the five wells have been used to correlate the wells for understanding the lateral and vertical variations in the stratigraphic layers. The correlation shows that the Datta Formation’s thickness increases at the centre of the basin whereas decreases on the east and south flanks of the basin. Reasons of Wells failure were concluded on the basis of the final well report and concluded that these well failure occur due to poor quality of the data and also due to some mechanical problems. Reservoircharacterization using statistical rock physics and petrophysics coupled with core data analysis can provide further insights into the hydrocarbon exploration.
机译:本研究专注于滩滩西部驻地巴基斯坦的一部分Bannu Basin的地质地质。为此目的,一些区域地震型材和深度探索性井数据已被用于集成。已经识别了十个Mappabale地震反射事件,其代表特定地质单位。一般而言,基于地震形成趋势,地平线浸入了研究区域的西北方向。由于沉积物朝向西北地区,该地区一般深化西北部。地震剖面MWI-83示出了界面的界面界面的偏置反向结构,该结构也被映射到双重轮廓图上。这可以被视为潜在的碳氢化合物涂层。区域地震型材在时间和深度域中的整个网格呈现,以获得地下各个地层单元的更清晰的图像。使用围网TWT的地震曲线的综合TWT制备了下倍频老化的Warcha砂岩的2D轮廓图,中三叠系老年的特写形成和早期Jurrasic老化的Datta形成。 DATTA形成和特雷德地层的时间和深度等高地图显示了在东南扭结的四方面粘附。计算封闭区域,大约为24平方米。此外,五孔的形成顶部已被用于与理解地层层中的横向和垂直变化相关联的孔。相关性表明,数据特拉形成的厚度在盆中的中心增加,而盆地的东部和南侧侧面减少。在最终井报告的基础上结束了井下失败的原因,得出的结论是由于数据质量差,因此由于某些机械问题,这些井失效也是如此。使用统计岩石物理学和岩石物理学与核心数据分析相结合的储层掩蚀性能可以进一步了解碳氢化合物勘探。

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