Abstract
The following subjects will be discussed in this article:
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The telescoping effect in the case of a juvenile fluid phase encountering a dense phase of peridotite, considered as an inevitable explanation of the genesis of the spilites.
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The relationship between lamprophyric rocks and spilitic rocks, the former being considered the dike-counterpart of the latter.
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The process of granitization interpreted as a possible reproduction of the spilitization mechanism on a capillary scale.
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Bibliographie Sommaire
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© 1974 Springer-Verlag Berlin · Heidelberg
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Tane, JL. (1974). Quelques Observations Nouvelles Relatives à la Genèse des Laves Spilitiques. In: Amstutz, G.C. (eds) Spilites and Spilitic Rocks. International Union of Geological Sciences, vol 4. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-88230-2_17
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DOI: https://doi.org/10.1007/978-3-642-88230-2_17
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