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• W2303863295 abstract "interface in shallow, tropical marine sediments. We conclude that during the very earliest stages of diagenesis, odinite peloids and infillings transformed to mixedJayer Sp-Ch, forming grain coatings with preservation of some of the original odinite textures. The formation of grain-coating Sp-Ch during early diagenesis apparently preserved high primary porosity in medium-grained specimens. Fine-grained and silty sandstones, however, contain poorly formed grain coatings and are tightly cemented by quartz, implying that grain size also has some effect on authigenic quartz growth. With increasing burial depth between 1702 and 6216 m, the proportion of Sp layers in Sp-Ch decreases from 20.7 ! 1.1 to 1.3 + 0.10/0, indicating that Sp layers transform to Ch layers with increasing diagenetic grade. The polytype of the Sp-Ch is essentially IDD at depths 2000 m, the polytype is randomly interstratified lbb-Iaa, and the proportion of IbD layers decreases from - 100 to 490lo over the interval studied. At depths 2000 m, orthohexagonal Sp transformstolaa Ch. There is essentially no change in Sp-Ch chemical composition with depth, implying that temperature is the dominant control on the structural transformations. Mean crystallite thickness also remains relatively constant with increasing depth, indicating that diagenetic transformations in Sp-Ch do not involve crystal-growth mechanisms typical of most clay minerals. Rather, the mineralogic transformations appear to proceed on a layer-byJayer basis, with individual layers dissolving and reprecipitating within the confines of the crystallites." @default.
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• W2303863295 date "1996-01-01" @default.
• W2303863295 modified "2023-09-27" @default.
• W2303863295 title "The origin and diagenesis of grain-coating serpentine-chlorite Tuscaloosa Formation sandstone, U.S. Gulf Coast" @default.
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• W2303863295 hasPublicationYear "1996" @default.
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