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Let's Make Outcrops Recover Their Value, Understanding the Rock on the Surface for Predicting Into the Subsurface: Woodford Shale Case Study, Ardmore Basin, Oklahoma

Abstract

Due to the high cost to acquire well cores along with today's low-oil-price scenarios, sizeable challenges are emerging especially for Previous HitunconventionalNext Hit reservoir characterization. Thus, detailed and Previous HitintegratedNext Hit outcrop data tied to well log responses provide means to understand shales on the surface and give supporting notions while predicting reservoir properties into the subsurface. In this work, first we present a multi-scale approach to characterize the vertical and lateral heterogeneities of a freshly Woodford Shale Outcrop in southern Oklahoma, the exposed succession is about 350 feet thick, comprising the entire Upper-Devonian Lower Mississippian Woodford Shale and partially the overlying Sycamore Limestone and underlying Hunton Group. About 14 detailed lithofacies were recognized, which relate direct observations and/or measurements such as color, texture, lithology, mineral assemblages and composition, bioturbation, presence and frequency of laminations and organic richness. Secondly, by cross-correlation with nearby well-logs and using clustering analysis a supervised electro-lithofacies classification was conducted, in which a statistical model was generated for permitting the prediction and propagation of up-scaled lithofacies in non-cored wells. In our case for the Ardmore Basin, the propagated model of lithofacies covers an area of about 64000 acres and includes well-logs information of 22 wells, depths of the Woodford shale in the subsurface range from 1000 to 3500 feet. The most remarkable outcrop-to-subsurface finding of this study is a laterally continuous cyclic pattern of two end-member groups of lithofacies: i) clay-rich, silica-poor, organic-rich, ductile lithofacies, and ii) clay-poor, silica-rich, carbonate-rich, brittle, fractured, organic-poor lithofacies. As if they were imitating a cyclic source-reservoir system, in which some lithofacies acts as oil/gas source and others as reservoirs or fracable rocks. Thickness and frequency of these cycles varies stratigraphically throughout the Woodford Shale, resulting in better gross intervals for Previous HitunconventionalNext Hit Previous HitresourcesTop within the Upper-Middle and Upper Woodford shale in the Ardmore basin.