Experimental constraints on evolution of leucite-basanite magma at 1 and 10-4 GPa: Implications for parental compositions of Roman high-potassium magmas

European Journal of Mineralogy

Volumn 21, Issue 4, 2009, Pages 763-782

  Conte, Aida Maria ^a   Dolfi, Daniela ^b   Gaeta, Mario ^a   Misiti, Valeria ^c   Mollo, Silvio ^b,c   Perinelli, Cristina ^d  

^a SAPIENZA UNIVERSITY OF ROME   (Italy)

^b ROMA TRE UNIVERSITY   (Italy)

^c ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

^d UNIVERSITY OF PISA   (Italy)

Author keywords

Experimental petrology; Limestone assimilation; Montefiascone Volcano; Roman Province; Ultrapotassic magma

Indexed keywords

ALUMINA; ALUMINUM OXIDE; CALCITE; CALCIUM OXIDE; CARBONATION; GLASS INDUSTRY; LIME; MAGNESIA; MICA; OLIVINE; OXIDE MINERALS; OXYGEN; POTASSIUM; SILICA; SILICON; TRACE ELEMENTS; VOLCANOES;

ANHYDROUS CONDITIONS; DIFFERENT PROPORTIONS; EXPERIMENTAL PETROLOGY; FRACTIONAL CRYSTALLIZATION; LIQUIDUS TEMPERATURE; MAJOR AND TRACE ELEMENTS; ROMAN PROVINCE; ULTRAPOTASSIC MAGMA;

ZEOLITES;

BASANITE; CHEMICAL COMPOSITION; CLINOPYROXENE; FRACTIONAL CRYSTALLIZATION; FUGACITY; LEUCITE; LIMESTONE; LOW PRESSURE; MAGMA; PETROLOGY; PHLOGOPITE; PRESSURE EFFECT; TRACE ELEMENT;

ITALY; LAZIO; MONTEFIASCONE; VITERBO;

EID: 73949110748     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2009/0021-1934     Document Type: Article

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