Partition coefficients determined from phenocryst and glass analyses of the climactic ejecta of Mount Mazama, Oregon View on Open Library

Partition coefficients determined from phenocryst and glass analyses of the climactic ejecta of Mount Mazama, Oregon

by Charles R Bacon

No reviews yet
First published: 1987 1 language
Subjects
Phenocrysts Volcanic ash, tuff

Reviews

Log in or sign up to write a review.

No reviews yet. Be the first!

More by Charles R Bacon

Geothermal resources in the Crater Lake area, Oregon

Geothermal resources in the Crater Lake ...

You Might Also Like

More in Phenocrysts
Phenocryst compositions of late ash-flow tuffs from the central San Juan caldera cluster

Phenocryst compositions of late ash-flow...

Peter W. Lipman
Feldspar and quartz phenocrysts in the Shingle Creek porphyry, British Columbia

Feldspar and quartz phenocrysts in the S...

H. H. Bostock
Genezis perlita

Genezis perlita

Phenocryst compositions of late ash-flow tuffs from the central San Juan caldera cluster

Phenocryst compositions of late ash-flow...

Peter W Lipman
A model to help explain Sr-isotope disequilibrium between feldspar phenocrysts and melt in large-volume silicic magma systems

A model to help explain Sr-isotope diseq...

Wendell A. Duffield
Relict plagioclase phenocrysts from metavolcanic rocks mantling a granite dome and the petrology of the associated rocks in the Grenville province of southeastern Ontario

Relict plagioclase phenocrysts from meta...

William Henry Spence