Quartz Cementation in Sandstones 2000
DOI: 10.1002/9781444304237.ch2
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The Origin of Large‐Scale Quartz Cementation: Evidence from Large Data Sets and Coupled Heat–Fluid Mass Transport Modelling

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Cited by 51 publications
(33 citation statements)
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“…Some older models of sandstone diagenesis invoked large-scale water flow systems as the main controls on reservoir quality (Giles et al 2000); these tended to assume relatively open geochemical systems. Some invoked a vital role for organic acids derived from source rocks (e.g.…”
Section: Open V Closed Systems and Secondary Porositymentioning
confidence: 99%
“…Some older models of sandstone diagenesis invoked large-scale water flow systems as the main controls on reservoir quality (Giles et al 2000); these tended to assume relatively open geochemical systems. Some invoked a vital role for organic acids derived from source rocks (e.g.…”
Section: Open V Closed Systems and Secondary Porositymentioning
confidence: 99%
“…Whilst this may apply to samples from very nearsource rock provenances, it would also require that the material derived from very discrete and homogeneous sedimentary layers. In part mitigation of this assumption, the scenario can exist where the diagenetic severity imparted upon a large area of sediment is uniform and the resultant diagenetic textures found on the quartz sand grains from the sample are therefore homogeneous throughout the sedimentary strata concerned [26].…”
Section: Grain Type Ratios Statistics and Grouping Techniques In Formentioning
confidence: 99%
“…Quartz cementation is the main cause of porosity loss in the Brae Formation sandstone reservoirs of the Miller and Kingfisher Fields (Giles et al, 2000;Marchand et al, 2000Marchand et al, , 2002. The precipitation of quartz overgrowths in many sedimentary basins commonly occurs during deep burial diagenesis (>2.5 km) at elevated temperatures, typically 70 -130 jC (e.g.…”
Section: Quartz Cementation Conditionsmentioning
confidence: 99%