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Diacritical Seismic Signatures for Complex Geological Structures: Case Studies from Shushan Basin (Egypt) and Arkoma Basin (USA)

机译:复杂地质结构的变径地震特征:以蜀山盆地(埃及)和阿科玛盆地(美国)为例

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Seismic reflection techniques show an imperative role in imaging complex geological structures and are becoming more acceptable as data interpreting tools in 2D/3D view. These subsurface geological structures provide complex seismic signature due to their geometrical behavior. Consequently, it is extremely difficult to interpret these seismic sections in terms of subsurface configuration. The main goal of this paper is to introduce seismic attributes as a powerful tool to interpret complex geological structures in different geological settings. In order to image these complex geological features, multiple seismic attributes such as coherence and curvature have been applied to the seismic data generated over the Shushan Basin (Egypt) and Arkoma Basin (USA). Each type of geological structure event usually generates a unique seismic “signature” that we can recognize and identify by using these seismic attributes. In Shushan Basin (Egypt), they provide a framework and constraint during the interpretation and can help prevent mistakes during a 3D structural modeling. In Arkoma Basin (USA), the seismic attributes results provide useful information for broader analyses of the complex structural relations in the region where the Ouachita orogenic belt intersects with the southern Oklahoma aulacogen. Finally, complex geological structures provide dramatically diacritical seismic signatures that can be easily interpreted by collaborating conventional seismic interpretation techniques with multiple seismic attributes.
机译:地震反射技术在成像复杂的地质结构中显示出必不可少的作用,并且越来越被人们视为2D / 3D视图中的数据解释工具。这些地下地质结构由于其几何行为而提供了复杂的地震信号。因此,很难根据地下构造来解释这些地震剖面。本文的主要目的是介绍地震属性,作为解释不同地质环境中复杂地质结构的有力工具。为了对这些复杂的地质特征进行成像,已将多个地震属性(如相干性和曲率)应用于在蜀山盆地(埃及)和阿科玛盆地(美国)上生成的地震数据。每种类型的地质结构事件通常都会产生一个独特的地震“特征”,我们可以通过使用这些地震属性来识别和识别这些特征。在蜀山盆地(埃及),它们在解释过程中提供了框架和约束,可以帮助防止在3D结构建模过程中出错。在美国的阿科玛盆地,地震属性结果为进一步分析沃基塔造山带与俄克拉荷马州奥拉库根南部的复杂结构关系提供了有用的信息。最后,复杂的地质构造提供了显着的变音地震特征,通过将传统的地震解释技术与多种地震属性结合起来可以轻松地解释这些特征。

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