Low-pressure phase equilibria of anhydrous anorthite-bearing mafic magmas

Author:

Kohut Edward J.1,Nielsen Roger L.2

Affiliation:

1. Department of Geosciences; Oregon State University; 104 Wilkinson Hall, Corvallis Oregon 97331 USA

2. Department of Geosciences and College of Oceanic and Atmospheric Sciences; Oregon State University; 104 Wilkinson Hall, Corvallis Oregon 97331 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference42 articles.

1. Petrology of lavas from the Lamont seamount chain and adjacent East Pacific Rise, 10°N;Allan;J. Petrol.,1989

2. Origin of compositional zonation (high alumina basaltic andesite) in the Giant Crater Lava Field, Medicine Lake Volcano, northern California;Baker;J. Geophys. Res.,1991

3. Water in subduction zone magmatism: New insight from melt inclusions in high-Mg basalts from central Mexico;Cervantes;Eos Trans. AGU,2000

4. Origin of high-An plagioclase in Tongan high-ca boninites: Implications for plagioclase-melt equilibria at low (PH2O);Danyushevsky;Can. Mineral.,1997

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