Please use this identifier to cite or link to this item: https://cris.library.msu.ac.zw//handle/11408/4607
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dc.contributor.authorChima, Priscilla-
dc.contributor.authorBaiyegunhi, Christopher-
dc.contributor.authorLiu, Kuiwu-
dc.contributor.authorGwavava, Oswald-
dc.date.accessioned2021-11-25T11:58:52Z-
dc.date.available2021-11-25T11:58:52Z-
dc.date.issued2018-
dc.identifier.issn2391-5447-
dc.identifier.urihttps://doi.org/10.1515/geo-2018-0059-
dc.identifier.urihttp://hdl.handle.net/11408/4607-
dc.description.abstractDiagenesis is one of the factors that affect reservoir quality in sandstones. Knowledge of diagenetic transformation and how it impacts the development of porosity in reservoirs rocks is thus key to successful mineral exploration. To date, little is known about the diagenesis of the uranium-hosted sandstones of the Stormberg Group, Karoo Basin, South Africa. Petrographic study, scanning electron microscopy (SEM) aided with energy dispersive X-ray (EDX), and X-ray diffraction (XRD) analyses were employed for the diagenetic study of the sandstones. This study aims to provide an account of the diagenesis of these rock units and how it impacts their reservoir quality. The diagenetic processes that have affected the sandstones are cementation, compaction, recrystallization, replacement, mineral overgrowth and dissolution. These processes have passed through early, late and uplift-related diagenesis. Formation of authigenic minerals and precipitation of the mineral cements occurred during different diagenetic phase but mostly during the early diagenetic stage. This stage was followed by lithification, which resulted in increased in grain packing, loss of pore spaces and thinning of bedding. Quartz and feldspar overgrowths, chloritization, muscovitization, concave-convex contacts, recrystallization, albitization and suture contacts are present in the late diagenetic stage. The uplift-related diagenetic stage was affected by calcitization, grain deformation and fracturing, dissolution and saussuritization. All these diagenetic processes largely affected the porosity and permeability of the sandstones. Primary and secondary porosities were both observed in the sandstones. In general, there is no single diagenetic process that is controlling the pattern of porosity evolution in the sandstones. On the other hand, the presence of fractured and dissolution pores tend to increase the porosity, thus enhancing the reservoir quality. This study shows that diagenesis has significantly altered the original petrologic characteristics of the sandstones which have induced considerable deterioration and heterogeneity in the reservoir quality of the Stormberg Group sandstones in the Main Karoo Basin of South Africa.en_US
dc.language.isoenen_US
dc.publisherDe Gruyter Openen_US
dc.relation.ispartofseriesOpen Geosciences;Vol. 10; No. 1: p. 740-771-
dc.subjectDiagenesisen_US
dc.subjectSandstonesen_US
dc.subjectReservoir qualityen_US
dc.subjectStormberg groupen_US
dc.subjectKaroo basinen_US
dc.titleDiagenesis and rock properties of sandstones from the Stormberg Group, Karoo Supergroup in the Eastern Cape Province of South Africaen_US
dc.typeArticleen_US
item.openairetypeArticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.grantfulltextopen-
item.languageiso639-1en-
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