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4. Diagenese von Kieselsedimenten und Hornsteinentstehung

verfasst von : Reinhard Hesse, Reinhard Gaupp

Erschienen in: Diagenese klastischer Sedimente

Verlag: Springer Berlin Heidelberg

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Zusammenfassung

Der Begriff Kieselsäurediagenese hat verschiedene Bedeutungen, da er verschiedene Prozesse der Diagenese beinhaltet. Er umfasst die Umwandlung leichter löslicher metastabiler in schwerer lösliche und schließlich stabile feste Kieselsäurephasen unter Wasserabgabe bei der Versenkungsdiagenese. Er bezeichnet ferner die Verdrängung durch Kieselsäure von ursprünglich nicht kieseligen Substanzen, besonders Karbonaten, Evaporiten, fossilem Holz oder vulkanischen Gesteinen, verursacht durch kieselsäureübersättigte Fluide einschließlich hydrothermaler Lösungen.

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Statt des üblichen Begriffs calcite compensation depth (CCD) wird hier calcite compensation level (CCL) gebraucht, um zu betonen, dass das Calcit-Kompensationsniveau im Ozean keine einheitliche Tiefenlage besitzt.

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Titel: Diagenese von Kieselsedimenten und Hornsteinentstehung
verfasst von: Reinhard Hesse
Reinhard Gaupp
Verlag: Springer Berlin Heidelberg
Buch: Diagenese klastischer Sedimente
Print ISBN: 978-3-662-59684-5

Electronic ISBN: 978-3-662-59685-2

Copyright-Jahr: 2021
DOI: https://doi.org/10.1007/978-3-662-59685-2_4