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Hydrothermale Mineral-Lagerstätten

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Zusammenfassung

Viele Mineral-Lagerstätten bilden sich nicht aus einem Magma, sondern aus hydrothermalen Fluiden, die genetisch mit Magmatismus verknüpft sein können aber nicht müssen. Während man unter dem Begriff „hydrothermal“ lediglich „heißer als die Umgebung“ versteht, ist der Begriff „Fluid“ für die meisten Erdwissenschaftler relativ unscharf definiert und beschreibt sowohl überkritische als auch unterkritische Lösungen, je nach Temperatur, Druck und chemischer Zusammensetzung, insbesondere dem Anteil der leichtflüchtigen Komponenten in dem betreffenden System. Hydrothermale Lagerstätten können in unterschiedlichen plattentektonischen Positionen innerhalb der Erdkruste und durch eine Reihe von Prozessen entstehen, von denen die folgenden besonders hervorzuheben sind.

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  1. Institut für Geographie und Geologie, Universität Würzburg, Würzburg, Deutschland

    Martin Okrusch & Hartwig E. Frimmel

  2. Department of Geological Sciences, University of Cape Town, Rondebosch, Südafrika

    Hartwig E. Frimmel

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Okrusch, M., Frimmel, H.E. (2022). Hydrothermale Mineral-Lagerstätten. In: Mineralogie. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-64064-7_23

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