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Stowell, H. H., Stein, E. (2005) THE SIGNIFICANCE OF PLAGIOCLASE-DOMINANT CORONAS ON GARNET, WENATCHEE BLOCK, NORTHERN CASCADES, WASHINGTON, U.S.A. The Canadian Mineralogist, 43 (1) 367-385 doi:10.2113/gscanmin.43.1.367

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Reference TypeJournal (article/letter/editorial)
TitleTHE SIGNIFICANCE OF PLAGIOCLASE-DOMINANT CORONAS ON GARNET, WENATCHEE BLOCK, NORTHERN CASCADES, WASHINGTON, U.S.A.
JournalThe Canadian Mineralogist
AuthorsStowell, H. H.Author
Stein, E.Author
Year2005 (February 1)Volume43
Issue1
PublisherMineralogical Association of Canada
Download URLhttps://rruff.info/doclib/cm/vol43/CM43_367.pdf+
DOIdoi:10.2113/gscanmin.43.1.367Search in ResearchGate
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Mindat Ref. ID64079Long-form Identifiermindat:1:5:64079:6
GUID0
Full ReferenceStowell, H. H., Stein, E. (2005) THE SIGNIFICANCE OF PLAGIOCLASE-DOMINANT CORONAS ON GARNET, WENATCHEE BLOCK, NORTHERN CASCADES, WASHINGTON, U.S.A. The Canadian Mineralogist, 43 (1) 367-385 doi:10.2113/gscanmin.43.1.367
Plain TextStowell, H. H., Stein, E. (2005) THE SIGNIFICANCE OF PLAGIOCLASE-DOMINANT CORONAS ON GARNET, WENATCHEE BLOCK, NORTHERN CASCADES, WASHINGTON, U.S.A. The Canadian Mineralogist, 43 (1) 367-385 doi:10.2113/gscanmin.43.1.367
In(2005, February) The Canadian Mineralogist Vol. 43 (1) Mineralogical Association of Canada

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