Microfacies Analysis of Limestones by Professor Dr. Erik Flügel (auth.)

By Professor Dr. Erik Flügel (auth.)

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By Professor Dr. Erik Flügel (auth.)

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Ooids, predominantly as superficial ooids with only a few laminae and a nucleus formed by large peloids. The ooids are partly micritized, therefore the lamination has been destroyed. Such micritized ooids are sometimes called "bahamite grains" (see Sect. 2); they occur chiefly in not too agitated environments. 3). Cat Cay, Great Bahama Bank. Thin-section. 5 mm 3. Large aggregate grain. Various sizes of large rounded micritic peloids are bonded by aragonitic micrite cement. Berry Islands, Great Bahama Bank.

X Chordata Tunicata ....................... X Vertebrata Fish Otolites ................... , caliche formation; mixing of various water zones, etc). Various groups of Recent organisms have different carbonate minerals in their shells (Table 2). The formation of Mg-calcite skeletons is influenced by the water temperature, the salinity, and the phylogenetic level of the organisms (Chave, 1954; Lowenstam, 1964). ; Sandberg, 1974). In contrast to their Recent analogs, Ancient ooids and perhaps also Ancient calcilutites seem to have been composed primarily of calcite rather than of aragonite.

Ass. , Oxford 20 (S) (S) (E) (RS) (E) (FI) (FI) (FI) (S) (C) Introduction to Facies Analysis Detailed description of morphology, sedimentology, diagenesis, organism distribution and Late Quaternary history of the Belize barrier reef east of Honduras. Of special interest is the description ofthe reeffront and the fore-reefslope. Klein, George deVries (1977): Clastic tidal facies. , 92 Figs. Champaign, Illinois: Continuing Education Publication Company Tidal sedimentary structure process-response models; Tidal paleocurrent models; Textural depositional models; Facies models; Occurrence of energy minerals (Petroleum, Uranium) in clastic tidal facies; Clastic tidal facies and geological history.

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