Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers

Nature

Volumn 411, Issue 6841, 2001, Pages 1037-1039

  Couch, S ^a   Sparks, R S J ^a   Carroll, M R ^b  

^a UNIVERSITY OF BRISTOL   (United Kingdom)

^b UNIVERSITY OF CAMERINO   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

CRYSTALS; MIXING; PETROLOGY; ROCKS;

EQUILIBRIUM CONDITIONS; REVERSELY ZONED CRYSTALS;

MINERALS;

MINERAL;

DISEQUILIBRIUM; LAVA; MAGMA CHAMBER; MINERALOGY;

ARTICLE; CHEMICAL COMPOSITION; COOLING; CRYSTAL; CRYSTALLIZATION; EQUILIBRIUM CONSTANT; HEATING; HIGH TEMPERATURE; PRIORITY JOURNAL; TEMPERATURE DEPENDENCE; THERMAL ANALYSIS; THERMODYNAMICS; VOLCANO;

MONTSERRAT;

EID: 0035963336     PISSN: 00280836     EISSN: None     Source Type: Journal    
DOI: 10.1038/35082540     Document Type: Article

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