Velocity Model Building Challenges And Solutions In The Eastern Mediterranean: Case Studies From The Region

A. El-Bassiony, J. Kumar, T. Martin, M. Bell
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Abstract

Recent large sub-salt discoveries in east Mediterranean waters have steered the focus on imaging beneath complex salt structures, where the main challenge is to correctly illuminate the sub-salt section. This involves optimizing acquisition parameters as well as building an accurate subsurface geological model. Only limited regions in the east Mediterranean are covered by multi-azimuth surveys; most of the 3D surveys available are narrow-azimuth. A lack of data diversity degrades the imaging of sub-salt zones even when using accurate subsurface models. Optimal model building for depth imaging involves the application of many complimentary imaging technologies to mitigate assumptions in any singular process. Illumination issues in the east Mediterranean are primarily caused by the complex interaction of shales and salt. The geometry of the salt layer and the velocity contrast across neighbouring lithologies determine the illumination and imaging quality beneath the salt layer. Using accurate interpretation of the top and base salt, and inserting a reliable velocity in the model, enhances the sub-salt imaging. This work focuses on the salt layer model building in three zones across the east Mediterranean Sea and the optimization of the salt/shales, and salt/carbonates velocities to enhance the sub-salt imaging and improve the reliability of amplitude data.
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在地中海东部建立速度模型的挑战和解决方案:来自该地区的案例研究
最近在东地中海海域发现的大型盐下油藏已经将重点转向了复杂盐结构下的成像,其中主要的挑战是如何正确地照亮盐下剖面。这包括优化采集参数以及建立准确的地下地质模型。只有东地中海的有限区域进行了多方位测量;大多数可用的三维测量都是窄方位角的。即使使用精确的地下模型,数据多样性的缺乏也会降低盐下层的成像。深度成像的最佳模型构建涉及许多互补成像技术的应用,以减轻任何单一过程中的假设。东地中海的照明问题主要是由页岩和盐的复杂相互作用引起的。盐层的几何形状和相邻岩性之间的速度对比决定了盐层下方的照明和成像质量。利用准确的顶盐和底盐解释,并在模型中插入可靠的速度,可以增强盐下成像。本文重点建立了东地中海三个区域的盐层模型,优化了盐/页岩、盐/碳酸盐的速度,以增强盐下成像,提高振幅数据的可靠性。
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