Cooling rate-induced differentiation in anhydrous and hydrous basalts at 500 MPa: Implications for the storage and transport of magmas in dikes

Author:

Del Gaudio P.,Mollo S.,Ventura G.,Iezzi G.,Taddeucci J.,Cavallo A.

Funder

INGV

FIRB MIUR

TRIGS

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference72 articles.

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2. Magmatic inclusions in silicic and intermediate volcanic rocks;Bacon;J. Geophys. Res.,1986

3. Quantification of H2O contents in silicate glasses using IR spectroscopy — a calibration based on hydrous glasses analyzed by Karl–Fisher titration;Behrens;Glass Sci. Technol.,2003

4. A combined rapid-quench and H2-membrane setup for internally heated pressure vessels: description and application for water solubility in basaltic melts;Berndt;Am. Mineral.,2002

5. The effect of water activity on the oxidation and structural state of Fe in a ferrobasaltic melt;Botcharnikov;Geochim. Cosmochim. Acta,2005

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