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Detailed petrophysical and geophysical characterization of core samples from the potential caprock-reservoir system in the Sulcis Coal Basin (Southwestern Sardinia - Italy)

机译:Sulcis煤盆地(西南撒丁岛-意大利)潜在盖层-储层系统岩心样品的详细岩石物理和地球物理特征

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摘要

In this work we present a methodology suitable to identify a caprock-reservoir system for the CO2 storage in the Sulcis Coal Basin (SW Sardinia - Italy). The petrophysical and geophysical characterizations indicate that the potential carbonate reservoir ("Miliolitico" Fm. Auct.) located at the base of the Eocene stratigraphic sequence in the mining district of the Sulcis Coal Basin, southwestern Sardinia, is heterogeneous but presents suitable reservoir zones for the storage of the CO2. The GPS data analysis indicates that the study area is stable, since it is characterized by a surface crustal deformation smaller than 1 mm/y.
机译:在这项工作中,我们提出了一种方法,用于确定在Sulcis煤盆地(西南撒丁岛-意大利)中二氧化碳封存的盖层-储层系统。岩石物理和地球物理特征表明,位于撒丁岛西南部Sulcis煤盆地采矿区始新世地层序列底部的潜在碳酸盐岩储集层(“ Miliolitico” Fm。Auct。)是非均质的,但具有合适的储集层区域二氧化碳的储存。 GPS数据分析表明研究区域是稳定的,因为其特征是地壳变形小于1 mm / y。

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