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Einführung

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Diagenese klastischer Sedimente

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Zusammenfassung

Diagenese ist die Summe aller Prozesse, durch welche aus Lockersedimenten verfestigte Sedimentgesteine werden. Diese Prozesse sind physikalischer, chemischer und biologischer Natur; sie verändern die mineralogische Zusammensetzung der Sedimentpartikel, ihre Textur und Anordnung im Sediment sowie insbesondere die Porosität und Permeabilität der Ablagerungen.

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Authors and Affiliations

  1. Dept. Geo- und Umjweltwissenschaften Sektion Geologie, Ludwig Maxilians Universität, München, Deutschland

    Reinhard Hesse

  2. Earth and Planetary Sciences, McGill University, Montreal, QC, Kanada

    Reinhard Hesse

  3. Institut für Geowissenschaften, Universität Jena, Jena, Deutschland

    Reinhard Gaupp

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  1. Reinhard Hesse
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  2. Reinhard Gaupp
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Correspondence to Reinhard Hesse .

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Hesse, R., Gaupp, R. (2021). Einführung. In: Diagenese klastischer Sedimente . Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-59685-2_1

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