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Mineralogie pp 305–310Cite as

Die Herkunft des Basalts

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Zusammenfassung

Basalte stellen die wichtigste Gruppe der vulkanischen Gesteine dar, die erdweit in großer Verbreitung auftreten. Bildung, Differentiation und Förderung basaltischer Magmen haben enge Beziehungen zur Plattentektonik (z. B. Pearce u. Cann 1973; Tabelle 19.1). Experimentelle Untersuchungen in vereinfachten Modellsystemen und an natürlichen Gesteinen haben entscheidend dazu beigetragen, die Entstehung von Basalt-Magmen durch partielle Anatexis von Peridotit im Oberen Erdmantel besser zu verstehen.

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Weiterführende Literatur

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Author information

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). Die Herkunft des Basalts. In: Mineralogie. Springer-Lehrbuch. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-34660-6_19

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  • DOI: https://doi.org/10.1007/978-3-642-34660-6_19

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  • Publisher Name: Springer Spektrum, Berlin, Heidelberg

  • Print ISBN: 978-3-642-34659-0

  • Online ISBN: 978-3-642-34660-6

  • eBook Packages: Life Science and Basic Disciplines (German Language)

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