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Sandsteindiagenese

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Diagenese klastischer Sedimente

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Zusammenfassung

Die Sandsteindiagenese ist das für praktische Anwendungen wichtigste Teilgebiet der Diagenese. Eigenschaften von Sandsteinen als Speichergesteine für Kohlenwasserstoffe, metallische Erze und Trinkwasser hängen grundlegend von ihrer Diagenese ab. Der wichtigste Teilaspekt der Sandsteindiagenese ist die Entwicklung des Porenvolumens während der Versenkungsdiagenese.

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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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Hesse, R., Gaupp, R. (2021). Sandsteindiagenese. In: Diagenese klastischer Sedimente . Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-59685-2_8

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