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Obsidian provenancing and magmatic fractionation in central oregon
D. I. Godfrey‐Smith
*
,
J. Kronfeld
, A. Strull
, J. M. D'Auria
*
Corresponding author for this work
School of the Environment and Earth Sciences
Dalhousie University
Nesher Cement Co
Simon Fraser University
Research output
:
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Article
›
peer-review
4
Scopus citations
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Keyphrases
Central Oregon
100%
Obsidian
100%
Magma Fractionation
100%
Chemical Difference
28%
Obsidian Sources
28%
Chemical Composition
14%
Chemical Variation
14%
Collection Site
14%
Small Region
14%
Geographic Region
14%
Late Miocene
14%
Endmember
14%
Natural Sources
14%
Magma Chamber
14%
K-Ar Dating
14%
Chemical Differentiation
14%
Geochemical Variation
14%
Difference Constraints
14%
Earth and Planetary Sciences
Fractionation
100%
Obsidian
100%
Oregon
100%
Geographic Areas
22%
Locale
11%
Miocene
11%
Magma Chamber
11%