Origin of minor and trace element compositional diversity in anorthitic feldspar phenocrysts and melt inclusions from the Juan de Fuca Ridge-Reference-Cited by-同舟云学术

Origin of minor and trace element compositional diversity in anorthitic feldspar phenocrysts and melt inclusions from the Juan de Fuca Ridge

Author:

Adams David T.¹,Nielsen Roger L.²,Kent Adam J. R.²,Tepley Frank J.³

Affiliation:

1. U.S. Geological Survey; Denver Federal Center; MS 973,; Denver; Colorado; 80225; USA

2. Department of Geosciences; Oregon State University; 104 Wilkinson Hall,; Corvallis; Oregon; 97330-5506; USA

3. College of Oceanic and Atmospheric Sciences; Oregon State University; 104 COAS Admin Bldg.,; Corvallis; Oregon; 97333-5503; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference78 articles.

2. Cr-rich spinels as petrogenetic indicators: MORB-type lavas from the Lamont seamount chain, eastern Pacific;Allan;Am. Mineral.,1988

4. Phenocrysts and glass inclusions and their bearing on oxidation and mixing of basaltic magmas, Kilauea Volcano, Hawaii;Anderson;Am. Mineral.,1972

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