Physical conditions of primitive tephritic magmas from vesuvius : first experimental results. - Archive ouverte HAL Access content directly
Conference Papers Year : 2004

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

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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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Dates and versions

hal-00078548 , version 1 (14-06-2006)

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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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