Titlebook: Microfacies of Carbonate Rocks; Analysis, Interpreta Erik Flügel Book 2010Latest edition Springer-Verlag GmbH Germany, part of Springer Nat

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Limestones are Biological Sediments,es by microbes and benthic encrusting organisms, and with the destructive role of micro- and macroborers. Knowledge of constructive and degrading processes is essential in evaluating carbonate budgets.

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Recognizing Paleoenvironmental Conditions,istribution of organisms. Section 12.1 summarizes paleoenvironmental proxies. Specific attention is given to paleoclimate-indicative criteria (Sect. 12.2) and to paleo-depth criteria (Sect. 12.3). The last section of this chapter deals with microfacies data that allow seismic events to be recognized.

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Basin Analysis: Recognizing Depositional Settings,e rocks, we focus on the diagnostic criteria for recognizing the facies characteristics needed in basin analysis studies. Microfacies is an important element of basin analysis, but must be applied along with all the other field and laboratory observations available for reconstructing depositional conditions.

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Practical use of microfacies: Reservoir Rocks and Host Rocks,cies analysis has been strongly triggered by the exploration and development of hydrocarbon reservoirs and source rocks in limestone and dolomites and is still of interest in understanding depositional controls, facies heterogeneities and reservoir property distribution

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