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Fluideinschlüsse in Mineralen

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Mineralogie

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Zusammenfassung

Viele Mineralkörner beinhalten unzählige Einschlüsse von Flüssigkeiten und/oder Gasen (Fluideinschlüsse), deren Größe typischerweise im Bereich von einigen Mikrometern liegt. Sie werden beim Wachstum oder der Rekristallisation des Wirtsminerals oder im Zuge dessen späterer Deformation und Verheilung hermetisch eingeschlossen. Mikrothermometrische Messungen sowie die direkte Analyse mittels Laser- und Ramanstrahlen, Gaschromatographie und Massenspektrometrie ermöglichen es, Informationen über Druck, Temperatur, Dichte und Zusammensetzung des Fluids und somit über die äußeren Zustandsbedingungen – sei es bei der Bildung des Wirtsminerals oder seiner späteren Alterationsgeschichte – zu gewinnen.

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Authors and Affiliations

  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

Authors
  1. Martin Okrusch
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  2. Hartwig E. Frimmel
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Correspondence to Martin Okrusch .

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© 2022 Springer-Verlag GmbH Deutschland, ein Teil von Springer Nature

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Okrusch, M., Frimmel, H.E. (2022). Fluideinschlüsse in Mineralen. In: Mineralogie. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-64064-7_12

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