Oceanic and continental basalts in the geochemical cycle |
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Authors: | Prof Dr W Nieuwenkamp |
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Institution: | (1) Vening Meinesz Laboratorium voor Geofysica en Geochemie, Rijksuniversiteit, Lucas Bolwerk 7, Utrecht, Holland |
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Abstract: | The apparently insignificant convergency of para- and ortho-amphibolites can explain the formation of enormous masses of basalt if brought in connection with the contrast between an oceanic basaltic and a granitic continental metabolism leading to a clear comprehension of the petrogenetic implications of the continuous rock series.
Zusammenfassung Die scheinbar bedeutungslose Konvergenz von Para- und Ortho-Amphiboliten reicht aus für die Erklärung der Herkunft von großen Basaltmengen, wenn der Unterschied zwischen ozeanischem basaltischem und kontinentalem granitischem Metabolismus berücksichtigt wird. Dies führt zur Klärung der wichtigsten Verhältnisse in der kontinuierlichen Gesteinsserie.
Résumé La convergence des amphibolites para et ortho explique bien la formation d'énormes masses de basalte, quand elle est mise en rapport avec le contraste entre le métabolisme basaltique oceanique et granitique continental. Il en résulte la signification pétrogénétique de la série continue des roches.
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