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Quick look cathodoluminescence analyses and their impact on the interpretation of carbonate reservoirs. Case study of mid-Jurassic oolitic reservoirs in the Paris Basin

机译:快速外观阴极发光分析及其对碳酸盐岩储层解释的影响。巴黎盆地中侏罗统蛇岩储层的案例研究

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Cathodoluminescence analyses on samples from Middle Jurassic oolitic limestones allow us to reconstruct the diagenetic history of these oil and gas reservoirs: a succession of events starting with the early, synsedimentary phases of marine cementation and ending with the addition of hydrocarbons to the reservoir. Constraints on the timing of events are derived from their calibration with the chronology of the well-known regional tectonic calendar.?Fracturing, due first to the post-Pyrenean extension and then to the Alpine compression, led respectively in Oligocene times to a recharge of the aquifer and a correlative change in cementation, and in Miocene times to the addition of hydrocarbons into the same flow units, this last event blocking diagenesis, at least in the zone above the oil-water contact. Distributions of cements and residual porosity within sedimentary units without stratigraphic significance, called here "pseudo-parasequences", were for the most part inherited from the original depositional facies.
机译:对中侏罗统橄榄岩石灰石样品的阴极发光分析使我们能够重建这些油气藏的成岩史:一系列事件始于海洋胶结作用的早期,沉积阶段,最后是向油气藏中添加了碳氢化合物。对事件时间的约束来自对它们的校准,并采用了著名的区域构造日历的时间顺序。压裂,首先是由于比利牛斯山脉的扩张,然后是由于高山压缩,在渐新世时期分别导致了含水层和胶结作用的相关变化,以及在中新世时期,碳氢化合物被添加到相同的流动单元中,最后这一事件至少在油水接触面以上的区域阻止了成岩作用。在没有地层学意义的沉积单元内,水泥的分布和残余孔隙度在这里被称为“伪副叠合序列”,大部分是从原始沉积相继承而来的。

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