1975
DOI: 10.1016/s0070-4571(08)71100-2
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Chapter 3 Diagenesis of Sandstones and Compaction

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Cited by 5 publications
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“…Some post depositional features following with chemical and physical changes occur in shale, effect the resistivity of shale to so much extent. Due to clay minerals digenesis, production of fresh water and also reduction of water salinity level occur [24,27]. This phenomena effect the salinity level and this reduces resistivity [28,29].…”
Section: Discussionmentioning
confidence: 99%
“…Some post depositional features following with chemical and physical changes occur in shale, effect the resistivity of shale to so much extent. Due to clay minerals digenesis, production of fresh water and also reduction of water salinity level occur [24,27]. This phenomena effect the salinity level and this reduces resistivity [28,29].…”
Section: Discussionmentioning
confidence: 99%
“…Such phenomena do not occur in the lower Nuttall Sandstone, as there is no banding and goethite is more than just a stain. Iron oxide can be diagenetic and form in the basin of deposition as detrital and authigenic iron bearing clay minerals break down (Greensmith 1989, Wolf & Chilingarian 1994, Pettijohn et al 1987. Clays readily absorb iron, and chlorite and smectite can contain iron in their lattices (Greensmith 1989, Pettijohn et al 1987.…”
Section: Analysis Of Primary and Secondary Cement In Lower Nuttall Samentioning
confidence: 99%
“…Arsenopyrite and pyrite in black shales above and below the lower Nuttall Sandstone or in lithic fragments of the sandstone itself may be the source of goethite, although XRD results indicate the surrounding shales are devoid of pyrite and arsenopyrite. If the goethite is locally sourced, a possible method for its precipitation is mentioned by Wolf & Chilingarian (1994) and Pettijohn et al (1987) and is outlined by Greensmith (1989): in a humid climate, iron may be released by hydrolysis into capillary pore water in rock exposed to the atmosphere. When such a situation occurs in the presence of a positive eH, iron is progressively oxidized and precipitated into pore space as goethite or hematite when it dewaters, which may lead to iron oxide concentrations of 1 to 5% in the host rock (Greensmith 1989).…”
Section: Analysis Of Primary and Secondary Cement In Lower Nuttall Samentioning
confidence: 99%
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