2018
DOI: 10.1016/j.marpetgeo.2017.12.026
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Evolution of porosity and pore geometry in the Permian Whitehill Formation of South Africa – A FE-SEM image analysis study

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Cited by 27 publications
(9 citation statements)
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“…Our observations regarding the evolution of porosity generally agree with the findings of Chukwuma et al (2018), who, using high-resolution FE-SEM imaging combined with EDS analyses found that porosity positively correlates with the degree of SOM maturation in Whitehill shales. However, we draw attention to one of their findings which stipulates that a drastic decrease in porosity is observed in some rocks linked to thermal decarboxylation of organic matter, correlating with the infilling of pores by fibrous grains (including carbonates, clays, silicates, and phosphates) generated by re-precipitation of framework grains previously dissolved by organic acid-rich fluids.…”
Section: Petrography Organic Particle Morphology Diagenesis and Porositysupporting
confidence: 91%
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“…Our observations regarding the evolution of porosity generally agree with the findings of Chukwuma et al (2018), who, using high-resolution FE-SEM imaging combined with EDS analyses found that porosity positively correlates with the degree of SOM maturation in Whitehill shales. However, we draw attention to one of their findings which stipulates that a drastic decrease in porosity is observed in some rocks linked to thermal decarboxylation of organic matter, correlating with the infilling of pores by fibrous grains (including carbonates, clays, silicates, and phosphates) generated by re-precipitation of framework grains previously dissolved by organic acid-rich fluids.…”
Section: Petrography Organic Particle Morphology Diagenesis and Porositysupporting
confidence: 91%
“…Intra-crystalline, organic porosity (e.g. Schieber et al, 2010;Chukwuma et al, 2018) has a much higher contribution to the rock porosity. Here, the inter-crystalline porosity is much lower compared to the KZF-1 shales, and, by contrast, the organic porosity, with a high degree of interconnectivity, controls the effective porosity of the rock.…”
Section: Petrography Organic Particle Morphology Diagenesis and Porositymentioning
confidence: 99%
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“…The samples were then coated with iridium and examined using field-emission scanning electron microscopy with an X-ray energy-dispersive detector (FEI Quanta 200F) to obtain high-resolution images and to determine the distribution of elements. More detailed procedures of the elemental, mineralogical, and microphotographic analyses can be found in a series of published references. …”
Section: Methods and Samplesmentioning
confidence: 99%
“…To analyse the optical characterization, a few methods were completed to confirm the properties of the ZnO Nps. The methods used were XRD analysis where the structure of hexagonal wurtzite of ZnO NPs can be observed [28], Field Emission Scanning Electron Microscopy (FE-SEM) analysis to determine the surface morphology, porosity, particle size of the ZnO NPs [29] and Fourier Transform Infrared (FTIR) Spectroscopy Analysis is to determine the polymeric properties of ZnO NPs by relying on infrared light to scan samples and observe bond properties [30]. Besides that, the Ultraviolet-visible spectroscopy (UV-vis) is used to determine the concentration of an analyte in a solution [31].…”
Section: Introductionmentioning
confidence: 99%