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Shales diagenesis

Berger G., Velde B., and Aigouy T. (1999) Potassium sources and illitization in Texas Gulf Coast shale diagenesis. J. Sedim. Res. 69, 151-157. [Pg.3646]

Evans I. J. (1989) Geochemical fluxes during shale diagenesis, an example from the Ordovician of Morocco. Water-Rock Interact. WRI-6, 219-222. [Pg.3648]

Evans J. (1990) Quartz dissolution during shale diagenesis implications for quartz cementation in sandstones. Chem. Geol. 84, 239-240. [Pg.3648]

ScHEGG, R. (1992) Coalification, shale diagenesis and thermal modelling in the Alpine Foreland basin the Western Molasse Basin (Switzerland/France). Org. Geochem., 18, 289-300. [Pg.161]

The main factors controlling a sandstone compaction are shales diagenesis and subsequent overpressures, the presence of evaporite formations which permit heat loss due to their high thermal conductivity, and early quartz overgrowths which resulted in a solid sandstone skeleton before Mesozoic subsidence. These overgrowths have impeded further reservoir compaction. Mapping such early quartz overgrowth devel-... [Pg.129]

CE Weaver. Geothermal alteration of clay minerals and shales diagenesis. Office of Nuclear Waste Isolation, 1979. [Pg.302]

Whittacker SG, Kyser TK (1990) Effects of sources and diagenesis on the isotopic and chemical composition of carbon and sulfur in Cretaceous shales. Geochim Cosmochim Acta 54 2799-2810... [Pg.277]

MURAtA (K.J.) and LARSON (R.R.), 1975. Diagenesis of Miocene siliceous shales, Tremblor Range, California. Journ. Res. U.S. Geol. Survey,... [Pg.203]

Chernoff, C.B. and Barton, M.D. (2001) Trace elements in black shale Fe-sulfides during diagenesis and metamorphism. Abstracts with Programs. The Geological Society of America, 33(6), 129. [Pg.204]

Fossil fuel resources a gaseous, liquid, or solid fuel material formed in the ground by chemical and physical changes (diagenesis, q.v.) in plant and animal residues over geological time natural gas, petroleum, coal, and oil shale. [Pg.433]

Clay mineral diagenesis also may play a role in dolomite formation during burial. The commonly observed conversion of smectites to illite can result in the release of the magnesium necessary for dolomite formation (e.g., McHargue and Price, 1982). Dolomite formation is observed near and within shale beds however, this process again appears to be a localized mechanism and probably is incapable of producing large quantities of dolomite. [Pg.389]

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See also in sourсe #XX -- [ Pg.395 ]



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Diagenesis

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