Trace element abundances in megacrysts and their host basalts: Constraints on partition coefficients and megacryst genesis

Geochimica et Cosmochimica Acta

Volumn 48, Issue 6, 1984, Pages 1201-1221

  Irving, Anthony J ^a   Frey, Fred A ^b  

^a UNIVERSITY OF WASHINGTON   (United States)

^b MASSACHUSETTS INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0021360950     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/0016-7037(84)90056-5     Document Type: Article

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87. Petrology and geochemistry of megacrysts, xenoliths, and their host basalts from the Terlingua mercury district of west Texas (abstract)
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109. Some experimentally determined zircon/liquid partition coefficients for the rare earth elements
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111. Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types
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114. Ultramafic inclusions and high pressure megacrysts from a nephelinite sill, Nandewar Mountains, northeastern New South Wales, and their bearing on the origin of certain ultramafic inclusions in alkaline volcanic rocks
115. An Al-spinel ultramafic-mafic inclusion suite and high pressure megacrysts in analcimite and their bearing on basaltic magma fractionation at elevated pressures
116. Structural and textural relationships of amphibole and phlogopite in peridotite inclusions. Dish Hill, California
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