Alaska Volcano Observatory | (super 10) Be and (super 9) Be in phenocryst and groundmass separates from Aleutian-arc volcanic rocks: implications for a magmatic origin of (super 10) Be in island-arc lavas

(super 10) Be and (super 9) Be in phenocryst and groundmass separates from Aleutian-arc volcanic rocks: implications for a magmatic origin of (super 10) Be in island-arc lavas

Author(s): Monaghan, M. C., Measures, C. I., Klein, Jeffrey, and Middleton, Roy

Publication Year: 1987

Bibliographic Reference:

Monaghan, M., Measures, C., Klein, J., and Middleton, R., 1987, (super 10) Be and (super 9) Be in phenocryst and groundmass separates from Aleutian-arc volcanic rocks: implications for a magmatic origin of (super 10) Be in island-arc lavas [abs.]: Eos, v. 68, n. 44, p. 1525.

Citation Updated: 2004-12-29 01:14:50

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