Petrophysical Properties of the Middle Jurassic Carbonates in the PICOREF Sector (South Champagne, Paris Basin, France)

J. Delmas, E. Brosse, P. Houel
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引用次数: 28

Abstract

This article, carried out as part of the PICOREF Project for the CO2 storage in the aquifers of the Paris Basin, presents an important petrophysical database from the numerous petroleum wells drilled in the PICOREF Sector (south-eastern part of the Paris Basin) between 1953 and 2001. These core data concern the three saline carbonated aquifers of the Middle Jurassic: the Oolithe Blanche and the Comblanchien formations, Upper Bathonian age, and the Dalle Nacree formation, Lower Callovian age, that would be used for the CO2 sequestration. Located at –1230 to –1750 m sub sea in the studied sector, these carbonate reservoirs which cumulative thickness is about 150 m, outcrop in the Burgundy region, at about 80 km south-eastern the Sector where they are exploited in several quarries. The analysis of the 6800 routine measurements (porosity and permeability) gathered for this study allowed to improve the knowledge of the petrophysical properties. Special measurements (mercury injection tests) allowed to characterize the porous medium.
法国巴黎盆地南香槟区PICOREF段中侏罗统碳酸盐岩岩石物理性质
本文是PICOREF巴黎盆地含水层二氧化碳封存项目的一部分,介绍了1953年至2001年间在PICOREF地区(巴黎盆地东南部)钻探的众多油井的重要岩石物理数据库。这些岩心数据涉及中侏罗世的三个含盐碳酸层:上Bathonian时代的Oolithe Blanche和Comblanchien组,以及下Callovian时代的Dalle Nacree组,它们将用于二氧化碳封存。这些碳酸盐岩储层位于研究区域海底-1230至-1750米处,累计厚度约为150米,露头在勃艮第地区,位于该区域东南约80公里处,在几个采石场开采。对本次研究收集的6800条常规测量数据(孔隙度和渗透率)进行分析,有助于提高对岩石物理性质的认识。可用于表征多孔介质特性的特殊测量(压汞试验)。
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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