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Einführung in die Geochemie

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Mineralogie

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Zusammenfassung

Bei der Lektüre dieses Buches ist dem aufmerksamen Leser klar geworden, dass die Verteilung der chemischen Elemente in der Natur wesentlich durch gesteinsbildende Prozesse kontrolliert wird. Bereits im frühen Entwicklungsstadium unseres Sonnensystems differenzieren sich die erdähnlichen Planeten, die ursprünglich chondritische Zusammensetzung hatten, in einen metallischen Kern und einen silikatischen Mantel. Krustenbildende Prozesse werden durch partielle Aufschmelzung im Mantel ausgelöst. Dabei entstehen Stamm-Magmen, in denen die inkompatiblen Elemente in verschiedenem Maße angereichert werden. Fraktionierte Kristallisation dieser Magmen, häufig kombiniert mit Assimilation von Nebengestein, führt zur Bildung magmatischer Serien von unterschiedlichem geochemischen Charakter.

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Authors and Affiliations

  1. Univ. Würzburg Mineralogisches Institut, Würzburg, Deutschland

    Professor Dr. Martin Okrusch

  2. Inst. Mineralogie, Univ. Würzburg Fak. Geowissenschaften, Würzburg, Deutschland

    Professor Dr. Siegfried Matthes

Authors
  1. Professor Dr. Martin Okrusch
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  2. Professor Dr. Siegfried Matthes
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Correspondence to Martin Okrusch .

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Okrusch, M., Matthes, S. (2014). Einführung in die Geochemie. In: Mineralogie. Springer-Lehrbuch. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-34660-6_33

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  • DOI: https://doi.org/10.1007/978-3-642-34660-6_33

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