Imaging Unconventional Reservoir Pore Systems
DOI: 10.1306/13592018m1123694
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Correlative X-ray and Electron Microscopy for Multi-scale Characterization of Heterogeneous Shale Reservoir Pore Systems

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Cited by 5 publications
(2 citation statements)
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“…High-resolution imaging techniques such as SEM and FIB-SEM provide insights into variations at the lamina and pore scales. Studying pore types is crucial for understanding pore network connectivity (permeability) and wettability, which control oil and water distribution and movement through pore spaces. Various pore types associated with different minerals and organic matter have been identified in mudrocks. ,, Loucks et al classified these into three general pore classes: interparticle pores (interP), intraparticle (intraP) pores within mineral crystals, and intraP organic matter (OM) pores. The formation of pores within the organic material of shales is intricately tied to their capacity to generate hydrocarbons, with this relationship influenced by the specific type of kerogen present in the rock and the thermal maturation of the organic material. ,, Moreover, Loucks et al found that OM pores in mudrocks develop when thermal maturation reaches an R o level of around 0.6% or higher, marking the onset of peak oil generation as per Dow and Kerogen .…”
Section: Introductionmentioning
confidence: 99%
“…High-resolution imaging techniques such as SEM and FIB-SEM provide insights into variations at the lamina and pore scales. Studying pore types is crucial for understanding pore network connectivity (permeability) and wettability, which control oil and water distribution and movement through pore spaces. Various pore types associated with different minerals and organic matter have been identified in mudrocks. ,, Loucks et al classified these into three general pore classes: interparticle pores (interP), intraparticle (intraP) pores within mineral crystals, and intraP organic matter (OM) pores. The formation of pores within the organic material of shales is intricately tied to their capacity to generate hydrocarbons, with this relationship influenced by the specific type of kerogen present in the rock and the thermal maturation of the organic material. ,, Moreover, Loucks et al found that OM pores in mudrocks develop when thermal maturation reaches an R o level of around 0.6% or higher, marking the onset of peak oil generation as per Dow and Kerogen .…”
Section: Introductionmentioning
confidence: 99%
“…Porosity and permeability of shales are often determined by examining core rock samples recovered from oil/gas wells drilled deep into rock formation. Recently, modern 2D/3D imaging techniques, have been used to investigate mineralogy and porosity in very fine detail, down to the sub-nanometer level [1][2][3][4] . These methods (and advanced image analysis) have facilitated characterization of the pore morphology within both the organic matter and non-organic (mineral) matrix of shales [5][6][7][8][9][10][11][12][13][14] .…”
mentioning
confidence: 99%