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Rezente Karbonatsedimentation

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Book cover Mikrofazielle Untersuchungsmethoden von Kalken

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Zusammenfassung

In den rezenten Meeren sind etwa 50% der Böden von Karbonatsedimenten bedeckt (Lisitzin, 1971). Bereiche bevorzugter Karbonatsedimentation sind die Flachmeere der Tropen und Subtropen zwischen 30°N und 30°S (Abb. 4) und der Tiefseeboden, dessen Fläche zu etwa 1/3 von Karbonatschlamm eingenommen wird.

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  1. Institut für Paläontologie, Universität Erlangen-Nürnberg, Loewenichstraße 28, D-8520, Erlangen, Bundesrepublik Deutschland

    Prof. Dr. Erik Flügel

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Flügel, E. (1978). Rezente Karbonatsedimentation. In: Mikrofazielle Untersuchungsmethoden von Kalken. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-08747-3_2

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  • DOI: https://doi.org/10.1007/978-3-662-08747-3_2

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