Gradients in silicic eruptions caused by magma mixing rather than chamber differentiation

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Autoria(s): Knesel, K. M.

Contribuinte(s)	K Knesel G Bergantz Jon Davidson
Data(s)	01/01/2001
Identificador	http://espace.library.uq.edu.au/view/UQ:95250
Publicador	Geological Society of America
Palavras-Chave	#EX #260301 Geochronology and Isotope Geochemistry #780104 Earth sciences
Tipo	Conference Paper