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Study of subsurface features using seismic reflection data in Erbil area, Kurdistan Region, Iraq

机译:使用地震反射数据研究伊拉克库尔德斯坦地区埃尔比勒地区的地下特征

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The present study seeks to interpret seismic reflection data for an area measuring approximately about 1,450 km~2 within the Erbil plain in the Kurdistan Region of Iraq to produce subsurface geological pictures. Thirteen seismic lines were identified by the Iraqi Oil Exploration Company using dynamite sources and then processed; then, a seismic line, BH-15, of around 432.5 km total length was used in this study. Three horizons (reflectors) were selected and identified by tying them directly to Demir Dagh well no. 1, these are H1, a reflector that represents the near top of the Lower Fars Formation; H2, a reflector that represents the top of the Pila Spi Formation; and H3, a reflector that represents the top of the Shiranish Formation. The qualities of the reflectors range between fair and good. All the isochrone and depth maps and 3D view pictures of the reflectors show the same main subsurface structural features trending in a NW-SE direction, namely, Erbil trough, Sherawa trough, and the southeastern plunge of the Demir Dagh anticline. Ninetyfive normal and reverse-type faults trending in a NW-SE direction were detected. Also, the maps show that the reflectors tend to increase in dipping and deepening towards the southeastern and eastern parts.
机译:本研究试图解释伊拉克库尔德斯坦地区埃尔比勒平原内约1,450 km〜2区域的地震反射数据,以产生地下地质图。伊拉克石油勘探公司使用炸药鉴定了13条地震线,然后进行了处理。然后,在这项研究中使用了总长度约为432.5公里的BH-15地震线。选择并确定了三个视域(反射器),方法是将它们直接与Demir Dagh井号10绑在一起。在图1中,它们是H1,代表下Fars组的顶部的反射器。 H2,代表Pila Spi地层顶部的反射器; H3是代表Shiranish地层顶部的反射器。反射镜的质量介于正常和良好之间。反射器的所有等时线图和深度图以及3D视图图片都显示出沿NW-SE方向趋向的相同主要地下结构特征,即Erbil槽,Sherawa槽和Demir Dagh背斜的东南倾角。检测到NW-SE方向上有95个正断型和反向型断层。此外,地图显示,反射器在向东南和东部倾斜和加深时趋于增加。

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