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Physical conditions of primitive tephritic magmas from vesuvius : first experimental results.

Abstract : Volatile-rich tephritic melts represent the most primitive compositions at Vesuvius. Recent eruptions (1906, 1944) record the multiple injections of such compositions at shallow levels, and their crystallization and mixing. Plinian magma chambers (eg, the 79 AD Pompei eruption) grow from the periodic supply of K-rich mafic melts.
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https://hal-insu.archives-ouvertes.fr/hal-00078548
Contributor : Nathalie Pothier <>
Submitted on : Wednesday, June 14, 2006 - 3:03:52 PM
Last modification on : Friday, April 5, 2019 - 8:08:24 PM
Long-term archiving on: : Monday, April 5, 2010 - 10:22:38 PM

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  • HAL Id : hal-00078548, version 1

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Michel Pichavant, Bruno Scaillet. Physical conditions of primitive tephritic magmas from vesuvius : first experimental results.. Geophysical Research Abstracts, 2004, Nice, France. ⟨hal-00078548⟩

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