Quantitatively Evaluating the Preservation of Deep-water Channel Architecture using 3D Synthetic Seismic from Outcrop

T. Langenkamp, L. Stright, S. Hubbard, B. Romans
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Abstract

Summary Forward seismic reflectivity models can be used to interpret depositional architecture and stratal surfaces. However, such studies often stop short at a qualitative assessment of the link between underlying depositional architecture and seismic resolvability, lacking a quantitative assessment. This study addresses this gap with a direct quantitative comparison of 3-dimensional facies architecture predicted from seismic with a “ground truth” to quantify heterogeneity facies associations and architecture preserved in inverted seismic data. The primary goal is to quantify how facies architecture information is preserved in and predicted from inverted seismic reflectivity data. The objective is to explore what the variables are that impact correct vs incorrect facies classification. With increasing seismic frequency, channel axis becomes harder to predict while mass transport deposits became easier to predict. Facies in shallow reservoirs are easier to predict than in deep reservoirs. Disorganized channel systems show greater facies predictability than organized systems due to greater AI contrasts. This study highlights what architectural information is preserved in 3-dimensional inverted seismic data, built from outcrop data of a deep-water system, which can aid directly in interpretation, reservoir prediction, and modelling.
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利用露头三维合成地震定量评价深水航道建筑的保存
正演地震反射率模型可以用来解释沉积构型和地层表面。然而,这类研究往往止步于对下伏沉积结构与地震可分解性之间的联系进行定性评估,缺乏定量评估。本研究通过将地震预测的三维相结构与“地面真实值”进行直接定量比较,以量化倒置地震数据中保存的非均质相关联和结构,从而解决了这一差距。主要目标是量化地震反射率数据中如何保存和预测相结构信息。目的是探索影响正确与不正确相分类的变量是什么。随着地震频率的增加,河道轴线的预测变得越来越困难,而体运沉积的预测变得越来越容易。浅层储层相比深层储层相更容易预测。由于AI对比较大,无序河道系统比有序河道系统表现出更强的相可预测性。这项研究强调了从深水系统的露头数据中建立的三维倒置地震数据中保留的建筑信息,这些信息可以直接帮助解释、储层预测和建模。
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