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New perspectives on Solid Earth Geology from Seismic Texture to Cooperative Inversion

机译:从地震构造到合作反演的固体地球地质新观点

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摘要

Seismic and electromagnetic methods are fundamental to Solid Earth research and subsurface exploration. Acquisition cost reduction is making dense 3D application of these methods accessible to a broad range of geo-scientists. However, the challenge of extracting geological meaning remains. We develop the concept of “textural domaining” for 3D seismic reflectivity data. Dip-steered seismic texture attributes are combined with unsupervised learning to generate sets of volume rendered images accompanied by a seismic texture reference diagram. These methods have the potential to reveal geological and geotechnical properties that would otherwise remain hidden. Analysis of seismic texture presents particular value in hard-rock settings where changes in velocity may be negligible across rock volumes exhibiting significant changes in rock mass texture. We demonstrate application and value of textural domaining with three industry-scale field examples. The first example links seismic texture to rock type along a 400 km long transect through central Australia. The second and third examples partition dense 3D seismic data based on texture for complex hard rock terrains in Nevada, USA and Kevitsa, Finland. Finally, we demonstrate application of domaining within texture guided cooperative inversion of 3D seismic reflectivity and magnetotelluric data to provide new perspectives on Solid Earth geology.
机译:地震和电磁方法是固体地球研究和地下勘探的基础。降低购置成本正在使广泛的地质学家可以轻松地将这些方法进行密集的3D应用。然而,提取地质意义的挑战仍然存在。我们为3D地震反射率数据开发了“纹理域”概念。浸入导向的地震纹理属性与无监督学习相结合,以生成带有地震纹理参考图的体积渲染图像集。这些方法具有揭示地质和岩土属性的潜力,而这些地质属性将不为人知。地震质地的分析在硬岩环境中具有特殊的价值,在这种情况下,整个岩石体积的速度变化可以忽略不计,从而显示出岩体质地的显着变化。我们通过三个行业规模的实例来说明纹理域的应用和价值。第一个示例通过澳大利亚中部沿400公里长的断面将地震质地与岩石类型联系起来。第二个和第三个示例根据美国内华达州和芬兰Kevitsa的复杂硬岩地形,根据纹理划分密集的3D地震数据。最后,我们展示了域划分在3D地震反射率和大地电磁数据的纹理引导协同反演中的应用,从而为固体地球地质学提供了新的视角。

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