Forward Stratigraphic Modeling of a Restored Cross Section from Apulia to Gavrovo

C. Pellan, P. Jiménez, R. Martín, B. Rubio de las Alas Pumariño, A. Chambers
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Abstract

Summary Building a coherent model, consistent with different events and processes over a long geological time frame is not an easy task. In this case study, The challenge was to model a 400 km long restored section in the Ionian zone (NW Greece), reproducing the main observations at wells and the key features seen on seismic and wells, in a single and reliable model of evolution of a Thethysian margin over more than two hundreds and fifty millions years. Furthermore, once the global conditions and the sedimentary dynamics of the evolution of this Passive Margin were defined by Forward Stratigraphic and Structural Modeling, a set of computation of Marine Organic Parameters was launched to address the main characteristics of the Source Rocks, improving the constrains on the Petroleum System. This large-scale integrated study brings notable and valuable information on the architecture of all the elements of the Petroleum System, from depositional conditions of Organic Rich layers to Reservoir size, continuity, connectivity, quality and EOD, and Seals thickness and efficiency. Finally, the Marine Organic Matter simulation helped to identify and characterize possible relevant Source Rocks layers.
Apulia - Gavrovo恢复剖面的正演地层模拟
在漫长的地质时间框架内,建立一个与不同事件和过程一致的连贯模型并不是一件容易的事。在这个案例研究中,我们面临的挑战是在爱奥尼亚地区(希腊西北部)建立一个400公里长的修复剖面,再现井中的主要观测结果以及地震和井中看到的关键特征,在一个单一的、可靠的忒提斯边缘演化模型中,超过两亿五千万年。通过正演地层与构造模拟,明确了被动边缘演化的整体条件和沉积动力学,启动了一套海相有机质参数的计算,以解决烃源岩的主要特征,改善了对含油气系统的约束。这项大规模的综合研究为油气系统的所有要素的结构提供了重要而有价值的信息,从富有机质层的沉积条件到储层的大小、连续性、连通性、质量和EOD,以及密封的厚度和效率。最后,海洋有机质模拟有助于识别和表征可能相关的烃源岩层。
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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