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From Source Rock to Reservoir: The Evolution of Self-Sourced Unconventional Resource Plays

机译:从烃源岩到储层:非常规自采资源的演化

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摘要

From a geological perspective, the exploration of shale source rocks is relatively straightforward. Advances in stimulation technologies, such as hydraulic fracturing, have made it possible to economically extract hydrocarbons, both liquid and gas, from their respective source rocks. However, the devil is in the details when it comes to "sweet spotting" which shale reservoirs are going to be the best producers. Organic-rich shales are fine grained and tend to be petrophysically challenging and mineralogically and geochemically heterogeneous on the nanoscale. The advent of focused ion beam - scanning electron microscopic (FIB-SEM) techniques now allows us to image the pore networks in the organic matter that generated the hydrocarbons we produce. Two types of pore networks exist in organic-rich shales. One type is water wetting and is associated with the inorganic component of the shale, mostly clays. The other pore network is hydrocarbon wetting and is associated with the porosity that develops in organic matter during maturation and hydrocarbon generation.
机译:从地质角度看,页岩烃源岩的勘探相对简单。诸如水力压裂之类的增产技术的进步使得从其各自的烃源岩中经济地提取液态和气态烃成为可能。然而,当涉及到“甜蜜发现”时,细节是魔鬼所在。页岩储层将是最好的生产者。富含有机物的页岩颗粒细小,在岩石物理上往往具有挑战性,并且在纳米尺度上在矿物学和地球化学上是异质的。聚焦离子束-扫描电子显微镜(FIB-SEM)技术的出现现在使我们能够成像产生有机碳氢化合物的有机物中的孔隙网络。富含有机物的页岩中存在两种孔隙网络。一种类型是水润湿,并且与页岩的无机成分(主要是粘土)有关。另一个孔隙网络是碳氢化合物润湿,并且与在成熟和碳氢化合物生成过程中有机质中形成的孔隙有关。

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