影响碳酸盐岩弹性特性的因素:两个案例研究和模拟结果的经验教训

F. Hong, F. Bastide, O. Zerhouni, C. Planteblat
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引用次数: 0

摘要

为了了解碳酸盐岩弹性特性的大散射,在两个不同的地质构造(来自澳大利亚的非热带碳酸盐岩和来自土耳其的实际大陆碳酸盐岩)中选择了两个数据集。三种统计方法旨在量化地质沉积环境和优势孔隙类型的影响,突出了石油弹性和岩石物理行为的异同。研究1表明,地质沉积环境信息可能是Vp变化的主要原因,而研究2中孔隙类型可能与纵波速度有很强的联系。为了了解这些异同的成因,并找出隐藏在地质意义中的共同信息,通过数字岩石进行了多次模拟试验,以量化碳酸盐微观结构孔隙体积分数、孔隙大小和孔隙形状的影响。数值模拟结果表明,孔隙尺寸对弹性响应无统计学影响;孔隙形态是影响材料弹性性能的主要参数之一。今后的工作是通过更多的模拟结果来了解岩石物理参数的影响因素。本研究的最终目的是确定影响地震速度的因素,然后利用它更好地解释地震反演的岩石物理参数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Factors Influencing Elastic Properties on Carbonate Rocks, Lessons Learnt from Two Case Studies and from Simulation Results
In order to understand the large scattering of elastic properties of carbonate rocks, two datasets were chosen in two different geological formations (non-tropical carbonate from Australia and actual continental carbonate from Turkey). Three statistical methods that aim to quantify the influence of Geological depositional environment and dominant pore type, that highlight similarities and differences on petro-elastic and petrophysic behaviors. Geological depositional environment information would be main reason for Vp variation as shown by Study 1, while in study 2 pore-type could have a strong link with P-wave velocity. To understand the origin of those similarities and differences, and to identify common information hidden inside the geological meanings, several simulation tests have been performed by digital rocks, in order to quantify the influences of the pore volume fraction, pore size and pore shape of carbonate microstructure. The numerical simulation shows that the pores size has statistically no influence on the elastic response; the pore shape is one of the main impacting parameter of the elastic properties. The future work consists on the understanding of influence factor for petrophysic parameter by more simulation results. The ultimate objective of this study is to identify factors that influence seismic velocity and then use it to better interpret the petrophysic parameters from seismic inversion.
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