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首页> 外文期刊>Journal of Petroleum Geology >GEOLOGICAL INTERPRETATION OF 2D SEISMIC REFLECTION PROFILES ONSHORE LEBANON: IMPLICATIONS FOR PETROLEUM EXPLORATION
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GEOLOGICAL INTERPRETATION OF 2D SEISMIC REFLECTION PROFILES ONSHORE LEBANON: IMPLICATIONS FOR PETROLEUM EXPLORATION

机译:黎巴嫩南部二维地震反射剖面的地质解释:对石油勘探的启示

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The first 2D seismic reflection acquisition onshore Lebanon was undertaken in 2013 by Spectrum Geo Ltd under the auspices of the Lebanese Ministry of Energy and Water. The surveys were recorded across a crustal-scale restraining bend in the central part of the Levant Fracture System. This contribution presents a geological interpretation of processed 2D data from the 2013 campaign. Two east-west trending seismic profiles were acquired and processed with a total linear distance of approximate to 80 km. Overall, a total of 16 key seismic reflectors were identified and mapped, and 20 faults were traced on the seismic profiles which were compared to geologic sections along the same acquisition path-lines. This helped to age-constrain the key reflectors and to assign the proper lithostratigraphic attributes to observed seismic packages. Interval velocities were determined every 500 m along each profile using the Dix equation to approximate the depth (in metres) for each time-picked horizon (ms), and ultimately to correlate seismic packages and measured thicknesses with known and/or extrapolated geologic rock units. The 50 km long SLEB-2D-01-13 profile (Batroun - Ainata, northern Lebanon) shows distinct seismic reflectors down to 2.5 seconds TWT. The deepest key reflector is believed to correspond to the middle Triassic evaporites which appear to have acted as a decoupling horizon. The interpreted profile displays the continuity of the overlying Qartaba structure, a potential viable exploration lead which merits further investigation. The 30 km long SLEB-2D-05-13 profile (Aley - Barr Elias, central Lebanon) shows excellent seismic imaging below the Bekaa valley, reaching 4 seconds TWT. The deepest key reflector is associated with the base-Jurassic horizon, 6300m to 8500m below ground level. Assumed Eocene platform carbonates underlie an interpreted Oligocene argillaceous package. These may form good hydrocarbon reservoir rocks if a viable petroleum system is present.
机译:在黎巴嫩能源和水利部的主持下,Spectrum Geo Ltd于2013年在黎巴嫩进行了首次二维地震反射采集。这些调查记录在黎凡特断裂系统中部的地壳尺度约束弯曲处。这项贡献对2013年战役中处理后的2D数据进行了地质解释。采集并处理了两条东西向的地震剖面,总线性距离约为80 km。总体上,总共确定并绘制了16个关键地震反射器,并在地震剖面上追踪了20个断层,并将这些断层与沿相同采集路径线的地质剖面进行了比较。这有助于限制关键反射器的年龄,并为观察到的地震包分配适当的岩石地层学属性。使用Dix方程确定沿每个剖面每500 m的间隔速度,以近似估计每个选定时间段(ms)的深度(以米为单位),并最终将地震包和测得的厚度与已知和/或外推的地质岩石单元相关联。 50 km长的SLEB-2D-01-13剖面图(黎巴嫩北部巴特伦-艾纳塔)显示了明显的地震反射波,反射波低至TWT 2.5秒。据信,最深的重点反射层对应于中三叠纪蒸发岩,似乎已经起到了解耦作用。解释后的剖面图显示了上覆的Qartaba结构的连续性,这是一个潜在的可行勘探线索,值得进一步研究。 30 km长的SLEB-2D-05-13剖面(黎巴嫩中部的Aley-Barr Elias)在Bekaa山谷下方显示了出色的地震成像,达到了TWT 4秒。最深的按键反射器与侏罗纪地层(距地面6300m至8500m)相关。假定始新世平台碳酸盐是解释的渐新世泥质包裹体的基础。如果存在可行的石油系统,它们可能会形成优质的油气藏岩石。

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