Kaersutite and Kaersutite eclogite from Kakanui, New Zealand - Water-Excess and Water-deficient melting to 30 kilobars

Bulletin of the Geological Society of America

Volumn 86, Issue 4, 1975, Pages 555-570

  Merrill, R B ^a,b   Wyllie, P J ^a  

^a UNIVERSITY OF CHICAGO   (United States)

^b Lunar and Planet Science Inst   (United States)

Author keywords

Experimental igneous petrology; Hornblende eclogite; Hydrous magma; Olivine basanite; Olivine nephelinite; Phase equilibria; Upper mantle; Volcanic breccia

Indexed keywords

BINARY ALLOYS; GARNETS; IGNEOUS ROCKS; LIQUIDS; MELTING; METAMORPHIC ROCKS; OLIVINE; PALLADIUM ALLOYS; PHASE EQUILIBRIA; PLATINUM ALLOYS; SILICA; SILVER ALLOYS; SODIUM COMPOUNDS; TITANIUM DIOXIDE;

BASANITE; ECLOGITES; HYDROUS MAGMA; UPPER MANTLE; VOLCANIC BRECCIA;

POTASSIUM COMPOUNDS;

BASANITE; BRECCIA; ECLOGITE; EXPERIMENTAL STUDY; HORNBLENDE; MAGMA; MELTING; NEPHELINITE; OLIVINE; P-T CONDITIONS; PHASE EQUILIBRIUM; PRESSURE EFFECT; UPPER MANTLE; WATER CONTENT;

KAKANUI; NEW ZEALAND; OTAGO; SOUTH ISLAND;

EID: 84875072286     PISSN: 00167606     EISSN: 19432674     Source Type: Journal    
DOI: 10.1130/0016-7606(1975)86<555:KAKEFK>2.0.CO;2     Document Type: Article

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