Two phases of sulphide saturation in Réunion magmas: Evidence from cumulates

Earth and Planetary Science Letters

Volumn 337-338, Issue , 2012, Pages 104-113

  Collins, S J ^a,b   Maclennan, J ^a   Pyle, D M ^c   Barnes, S J ^d   Upton, B G J ^e  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^b DURHAM UNIVERSITY   (United Kingdom)

^c UNIVERSITY OF OXFORD   (United Kingdom)

^d UNIVERSITÉ DU QUÉBEC À CHICOUTIMI   (Canada)

^e UNIVERSITY OF EDINBURGH   (United Kingdom)

Author keywords

Magmatic sulphides; R union; Trace metals; Volcanic degassing

Indexed keywords

ACTIVE VOLCANOES; ATMOSPHERIC MONITORING; CHALCOPHILE ELEMENTS; COMBINED ANALYSIS; GAS COMPOSITIONS; GAS TRANSFER; GASPHASE; HIGH DENSITY; MAGMATIC EVOLUTION; MAGMATIC SULPHIDE; MELT FORMATION; MELT INCLUSIONS; SULPHUR CONCENTRATION; TITANOMAGNETITES; TRACE METAL; TRACE METAL CONCENTRATION; ULTRAMAFIC CUMULATE; VOLCANIC DEGASSING; VOLCANIC SYSTEMS;

DEGASSING; MINERAL EXPLORATION; SULFUR; VOLCANOES;

SULFUR COMPOUNDS;

CUMULATE; DEGASSING; FRACTIONAL CRYSTALLIZATION; GABBRO; IMMISCIBILITY; MAGMA; MAGMATISM; MELT INCLUSION; SULFIDE; TITANOMAGNETITE; TRACE METAL; VOLCANIC ERUPTION; VOLCANO;

EID: 84862644054     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.05.027     Document Type: Article

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