Forward Model Applied to Channelized Turbidite Systems: A Case Study of the Benin Major Valley Fill

M. Lemay, F. Ors, J. Grimaud, J. Rivoirard, I. Cojan, X. Freulon
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Abstract

Channelized turbidite systems are associated with extensive hydrocarbon reservoirs. Yet building realistic turbidite reservoir models is still a challenge. We take advantage of some similarities between fluvial and turbidite environments to transpose the Flumy model , initially dedicated to fluvial reservoirs (Lopez al., 2008), to channelized turbidite systems by simulating the main processes at play in the submarine realm : channel lateral migration, avulsion, aggradation, overflowing, flow stripping, and sediment transport (Lemay 2018). A flow compatible with the input channel geometry parameters is first built. This flow controls the channel evolution through time and thus the stratigraphic architecture of deposits, as well as their grain size. In this study, we present the application of Flumy to the case study of the Benin major valley .
水道化浊积体系的正演模型应用:以贝宁大河谷填充物为例
河道化浊积岩体系与广泛的油气藏相联系。然而,建立真实的浊积岩储层模型仍然是一个挑战。我们利用河流和浊积岩环境之间的一些相似之处,通过模拟海底领域的主要过程,将最初专门用于河流储层的fluy模型(Lopez al., 2008)转换为河道化浊积岩系统:河道横向迁移、撕脱、淤积、溢水、流剥和沉积物运输(Lemay 2018)。首先建立了与输入通道几何参数兼容的流。这种水流控制着河道随时间的演变,从而控制着沉积物的地层结构,以及它们的粒度。在本研究中,我们介绍了Flumy在贝宁大河谷案例研究中的应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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