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Orthomagmatische Erzlagerstätten

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Mineralogie

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Zusammenfassung

Zunächst seien einige allgemeine Bemerkungen zur Genese und Gliederung von Lagerstätten vorausgeschickt: Durch magmatische Prozesse (Plutonismus und Vulkanismus) können Schwer metalle oder andere geochemisch seltene Elemente über den geochemischen Durch schnitt der Erdkruste angereichert werden. Es kommt zur Kristallisation von Erz- und Industriemineralen, die bauwürdige oder sogar weltwirtschaftlich bedeutsame Erzund Minerallagerstätten bilden können.

†Deceased

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Okrusch, M., Matthes †, S. (2010). Orthomagmatische Erzlagerstätten. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_19

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