Reframing Exploration Workflows for Small to Super-Merge 3D Seismic Interpretation

David J. A. Taylor, Sadaqat S. Ali
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Abstract

Techniques for 3D seismic interpretation by geoscientists are continuously undergoing improvements, and future exploration is anticipated to continue to benefit from high-confidence first pass interpretations utilizing all of the available seismic and well data. Workflows have been developed on a ‘super-merge’ 3D volume to produce attribute-enhanced chronostratigraphic stratal surfaces, allowing interpretation of regional-scale seismic facies and associated seismic geomorphology and tectonostratigraphy. In this example, a semi-supervised machine-based learning workflow has provided rapid turnaround interpretation of the structural framework and chronostratigraphy throughout the entire 3D seismic volume, maximizing the value of the seismic information. This workflow consists of a three-step auto-tracking workflow to build a Relative Geological Time (RGT) geo-model directly from the seismic volume. This enables more time to spend on geological validation and interpretation of the stratal surface seismic geomorphology. Study results have provided the foundation for rapid turnaround well and seismic integrated play fairway maps; a powerful tool for stimulating exploration in mature areas or wildcat acreage assessment. This study focused on Middle and Upper Jurassic carbonates deposited on a broad low angle platform on the Arabian Plate. Interpreting in map view on RGT constrained stratal surfaces with attributes such as, relative acoustic impedance and spectral decomposition, is invaluable for visualization since the stratal surface follows the morphology of the imaged geologic features. The ability to select any stratal surface within the volume and flatten, either on a seismic display or the Relative Geological Time geo-model, is particularly useful to establish the timing of major tectonic episodes and accommodation space fluctuations.
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小到超合并三维地震解释的重构勘探工作流程
地球科学家的三维地震解释技术正在不断改进,预计未来的勘探将继续受益于利用所有可用地震和井数据的高可信度首次解释。在“超级合并”三维体上开发了工作流程,以生成属性增强的年代地层地层面,从而可以解释区域尺度的地震相以及相关的地震地貌和构造地层学。在这个例子中,基于半监督的机器学习工作流程在整个三维地震体中提供了结构框架和年代地层的快速周转解释,最大限度地提高了地震信息的价值。该工作流由三步自动跟踪工作流组成,直接从地震体中构建相对地质时间(RGT)地质模型。这使得更多的时间花在地层地表地震地貌的地质验证和解释上。研究结果为快速周转井和地震综合球道图的绘制提供了依据;在成熟地区刺激勘探或野猫面积评估的有力工具。本研究集中研究了沉积在阿拉伯板块宽低角台地上的中、上侏罗统碳酸盐岩。利用相对声阻抗和光谱分解等属性在RGT约束下的地层表面的地图视图中进行解释,对于可视化来说是非常宝贵的,因为地层表面遵循成像地质特征的形态。在地震显示或相对地质时间地质模型上选择体积内的任何地层表面并将其平坦化的能力,对于确定主要构造事件和可容纳空间波动的时间特别有用。
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