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Three-dimensional seismic-based lithology prediction using impedance inversion and neural networks application: Case-study from the Mannville Group in East-Central Alberta, Canada.

机译:基于阻抗反演和神经网络的基于地震的三维岩性预测:来自加拿大东中亚艾伯塔省曼维尔小组的案例研究。

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摘要

The Lower Cretaceous Mannville Group in East-Central Alberta is one of the main targets for hydrocarbon exploration in Western Canada, typically associated with stratigraphic controls. The depositional environment is diverse, ranging from fluvio-continental to shallow marine. Mannville Group strata overlie a major unconformity that separates them from predominantly carbonate rocks of the Paleozoic (Devonian). This study sought to integrate well and 3-D seismic data to create a stratigraphic architecture for the zone of interest. Seismic inversion was applied to the data and proved to be an excellent tool for mapping the unconformity, clearly distinguishing between the clastic rocks above, and the units below. The inversion result was included as part of a seismic attribute study applied to the dataset. Stepwise regression and validation testing indicated that a combination of six attributes was found to provide the best set able to predict log-derived physical properties related to lithology (gamma-ray) using the seismic data. This result was used to train a neural network, and finally, a pseudo-lithology volume able to estimate the distribution of lithology within the Mannville Group over the whole 3-D survey was generated. New stratigraphic features that were non-apparent in the original amplitude seismic version were discovered using the inversion and the pseudo-lithology volumes. The results of this study show how comparing the three different 3-D seismic versions can be useful for understanding the stratigraphic complexity of the Mannville. The extensive methodology approach presented herein can be used for analog purposes in Western Canada as well as in any other geological setting.
机译:艾伯塔省中东部的下白垩统曼维尔组是加拿大西部油气勘探的主要目标之一,通常与地层控制有关。沉积环境是多种多样的,从潮汐大陆到浅海。曼维尔集团地层上覆有一个主要不整合面,将其与古生界(德文系)的碳酸盐岩分开。这项研究试图整合井眼和3D地震数据,以建立感兴趣区域的地层构造。地震反演应用于数据,并被证明是绘制不整合面的绝佳工具,可以清楚地区分上方的碎屑岩和下方的碎屑岩。反演结果包括在应用于数据集的地震属性研究中。逐步回归和验证测试表明,发现六个属性的组合可提供最佳集合,该集合能够使用地震数据预测与岩性(γ射线)有关的对数派生物理性质。这个结果被用来训练一个神经网络,最后,生成了一个能够估计整个3D调查中Mannville组内岩性分布的伪岩性体。使用反演和伪岩性体发现了在原始振幅地震版本中不明显的新地层特征。这项研究的结果表明,比较三种不同的3D地震版本如何有助于理解曼维尔的地层复杂性。本文介绍的广泛方法论方法可以在加拿大西部以及任何其他地质环境中用于模拟目的。

著录项

  • 作者

    Smaili, Melik A.;

  • 作者单位

    McGill University (Canada).;

  • 授予单位 McGill University (Canada).;
  • 学科 Geology.Geophysics.
  • 学位 M.Sc.
  • 年度 2009
  • 页码 76 p.
  • 总页数 76
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:38:26

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