Titlebook: Carbonate Facies in Geologic History; James L. Wilson Textbook 1975 Springer-Verlag Berlin · Heidelberg 1975 Fazies.Gestein.Jura.Karbonatg

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Fernando Corinto,Mauro Forti,Leon O. Chuae persistence of platforms situated just at sea level, the tectonic activity which provided periodic incursions of terrigenous clastics, and the enhanced possibilities of eustatic sea-level fluctuations (either glacially or tectonically induced) all coincided to make this time in earth history favorable for cyclic sedimentation.

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0172-6234 ory of science. This is true in all the diverse fields of carbonate geology: the study of Recent environments, marine zoology and botany, organic geochemistry, trace element and isotope geochemistry, mineralogy, microfacies of depositional environments, and trace-fossil and sedimentary structure inv

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Permo-Triassic Buildups and Late Triassic Ecologic Reefs,ugh, they still present unsolved problems of origin and subsequent diagenetic history. This Chapter briefly reviews and compares these famous models of carbonate facies focusing on both the deposition and diagenesis of the sediments.

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https://doi.org/10.1007/978-3-030-64977-7of clear, warm, shallow water. A world map (Fig. I-1) showing areas of modern carbonate deposition demonstrates clearly a positive correlation between such deposition and the equatorial belt and areas of warm ocean currents. Fairbridge (Chilingar et al., 1967, p. 404) presented a graph showing that

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Luca Patanè,Roland Strauss,Paolo Arenae geologic record. These patterns recur in a variety of tectonic settings. This Chapter considers these interrelations and also treats correlation problems in carbonate strata and the techniques for recognition of approximate “time planes” in shelf and shelf-margin areas. The Chapter contains many o