Fully Integrated Modelling of Subsurface, Remote Sensing and Outcrop Geology; Prospect Generation in the Paleozoic of the Ahnet Basin Algeria

J. V. Dijk, H. Guney
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Abstract

The fully integrated modelling of subsurface seismic and well data with outcropping surface geological data is a challenge in which the application of modern technologies which involves the standardisation of datasets on different scales and from different sources plays a key role. In this paper we present an example of the Paleozoic of the Ahnet Basin in Algeria where a prospect generation exercise was undertaken integrating data from 2d and 3d seismic volumes, logs and core data from previously drilled wells, maps of outcropping geology, and high-resolution remote sensing datasets. The geology of the area is well known from previous studies on both surface geology and well data, and comprises a Paleozoic series unconformably resting on infra-Cambrian relative basement, and made up of clastic sedimentary series with intercalation of limestone sediments ranging from Cambrian to Devonian Age, which comprise various gas bearing tight reservoirs some of which producing in this part of the Basin. These are present in anticlinal structures of Hercynian Age which are partly eroded and covered by Cretaceous bioclastic limestones. The anticlines show a deformational history reflecting an interference of differently oriented Hercynian transpressional deformation patterns overprinted by later stage, Alpine reactivations. Our integrated geological analyses permitted to propose a new updated view on the geological history of the area. This includes the reconstruction of the structural deformation of the Hercynian anticlines, and the reconstruction of the post-Hercynian geological evolution including structural reactivation, showing tilting and upheaval of the area in Alpine and Recent times. An extensive interpretation of outcropping geological structures was performed using high resolution satellite images and specific image processing. This was calibrated with available high-quality geological maps and some later additional limited geological surveys. Detailed well log correlations and seismic interpretation 2d and 3d seismic data provided a detailed framework of subsurface structures. The datasets on surface vand subsurface originally coming from different digital sources were integrated in one uniform interpretation environment using best practice standardization which permitted to drive the seismic interpretation and depth modelling, by carefully calibration with outcropping features such as bedding dip, fault trends and fold axis trends. Applying regional velocity modelling this permitted to correctly map the geological structures and prospects in the area, and perform an articulated exercise of Prospective and Contingent Resources estimates. The application of an integrated geoscientific workflow deploying up-to-date technologies which integrate GIS with a surface-subsurface 3d modelling space shows the validity of new developments of the 4th Industrial Revolution in the planning of E&P Prospect evaluation.
地下、遥感和露头地质完全一体化建模阿尔及利亚Ahnet盆地古生界远景世代
地下地震和井数据与露头地表地质数据的完全集成建模是一个挑战,其中涉及不同尺度和不同来源数据集标准化的现代技术的应用起着关键作用。在本文中,我们以阿尔及利亚Ahnet盆地的古生代为例,在该盆地进行了远景生成练习,整合了2d和3d地震数据、以前钻探井的测井和岩心数据、露头地质图和高分辨率遥感数据集。从以往的地面地质和井资料的研究来看,该区的地质情况是已知的,包括一个位于下寒武统相对基底上不整合的古生代系列,由寒武系至泥盆系的碎屑沉积系列和灰岩沉积物的夹层组成,这些沉积系列包括各种含气致密储层,其中一些储层在盆地的这一部分生产。它们存在于海西期背斜构造中,部分被白垩纪生物碎屑灰岩侵蚀和覆盖。背斜的变形历史反映了不同方向的海西期挤压变形模式的干扰,叠加了后期的阿尔卑斯再激活。我们的综合地质分析使我们能够对该地区的地质历史提出一个新的更新的观点。这包括海西期背斜构造变形的重建,以及海西期后地质演化的重建,包括构造活化,显示了该地区在高山期和近世的倾斜和隆起。利用高分辨率卫星图像和特定的图像处理,对露头地质构造进行了广泛的解释。这是用现有的高质量地质图和后来一些额外的有限地质调查来校准的。详细的测井对比和地震解释2d和3d地震数据提供了地下结构的详细框架。地面和地下的原始数据集来自不同的数字来源,使用最佳实践标准化集成在一个统一的解释环境中,通过仔细校准露头特征(如层理倾角、断层趋势和褶皱轴趋势),可以驱动地震解释和深度建模。应用区域速度模型,可以正确绘制该地区的地质结构和前景图,并进行远景资源和潜在资源估算。综合地球科学工作流程的应用,将GIS与地表-地下三维建模空间相结合,展示了第四次工业革命新发展在勘探开发前景评估规划中的有效性。
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