盐下储层细颗粒评价

T. M. Castro, W. Lupinacci
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引用次数: 6

摘要

桑托斯盆地盐下碳酸盐岩储层的表征面临许多挑战。在地球物理测井分析的基础上,提出了Barra Velha组和Itapema组储层特征,强调了细颗粒的存在对储层的影响。分析井结果表明,Itapema组和Barra Velha组是Buzios油田的勘探目标。Itapema组受细颗粒产状的影响较小,其孔隙特征优于Barra Velha组。细颗粒的存在对Barra Velha Fm储层产生了很大的负面影响,严重影响了测井曲线的响应,影响了储层的质量。有鉴于此,我们提出Barra Velha Fm凹陷相划分为下凹陷和上凹陷。这种划分是基于细颗粒沉积的末端。测井资料显示,将上裂谷期与凹陷期分开的阿拉戈斯内部不整合与细颗粒沉积的开始有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of fine-grains in pre-salt reservoirs
Pre-salt carbonates of the Santos Basin represent many challenges in the characterization of their reservoirs. This paper proposes the reservoir characterization of the Barra Velha and Itapema Formations based on the analysis of geophysical well logs, highlighting the influence of fine-grains presence. In the analyzed well, the results show that the Itapema and Barra Velha Formations are the exploratory targets in the Buzios Field. The Itapema Fm is less influenced by the occurrence of fine-grains, and presents better permo-porous characteristics than in the Barra Velha Fm. The presence of fine-grains causes a great negative impact on the Barra Velha Fm reservoir, affecting substantially the response of the well logs and compromising the reservoir quality. Due to this behavior, we propose the Barra Velha Fm sag phase division into Lower Sag and Upper Sag. This division is grounded at the end of fine-grain deposition. In its turn, the intra-Alagoas unconformity which separates the Upper Rift phase from the Sag phase, in the well logs, was correlated with the beginning of fine-grains deposition.
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