کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
8141737 1523834 2016 18 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Integration between well logging and seismic reflection techniques for structural analysis and reservoir characterizations, Abu El Gharadig basin, Egypt
ترجمه فارسی عنوان
ادغام بین روش های ورود به سیستم و روش بازتاب لرزه ای برای تحلیل ساختاری و خصوصی سازی مخزن، حوضه ابو الغرادیق، مصر
کلمات کلیدی
کویر غربی، حوضه ابو الغرادیق، مخزن خوب ورود لرزه ای،
موضوعات مرتبط
مهندسی و علوم پایه فیزیک و نجوم نجوم و فیزیک نجومی
چکیده انگلیسی
Abu El Gharadig basin is located in the northern part of the Western Desert, Egypt. Geophysical investigation in the form of thirty (3D) seismic lines and well logging data of five wells have been analyzed in the oil field BED-1 that is located in the northwestern part of Abu El Gharadig basin in the Western Desert of Egypt. The reflection sections have been used to shed more light on the tectonic setting of Late Jurassic-Early Cretaceous rocks. While the well logging data have been analyzed for delineating the petrophysical characteristics of the two main reservoirs, Bahariya and Kharita Formations. The constructed subsurface geologic cross sections, seismic sections, and the isochronous reflection maps indicate that the area is structurally controlled by tectonic trends affecting the current shape of Abu El Gharadig basin. Different types of faults are well represented in the area, particularly normal one. The analysis of the average and interval velocities versus depth has shown their effect by facies changes and/or fluid content. On the other hand, the derived petrophysical parameters of Bahariya and Kharita Formations vary from well to another and they have been affected by the gas effect and/or the presence of organic matter, complex lithology, clay content of dispersed habitat, and the pore volume.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: NRIAG Journal of Astronomy and Geophysics - Volume 5, Issue 2, December 2016, Pages 362-379
نویسندگان
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