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Borisenko, L. F., Борисенко, Λ. Φ. (1967) Trace elements in pyroxenes and amphiboles from ultramafic rocks of the Urals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 403-410 doi:10.1180/minmag.1967.036.279.10

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Reference TypeJournal (article/letter/editorial)
TitleTrace elements in pyroxenes and amphiboles from ultramafic rocks of the Urals
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsBorisenko, L. F.Author
Борисенко, Λ. Φ.Author
Year1967 (September)Volume36
Issue279
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-279-403.pdf+
DOIdoi:10.1180/minmag.1967.036.279.10Search in ResearchGate
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Mindat Ref. ID6091Long-form Identifiermindat:1:5:6091:6
GUID0
Full ReferenceBorisenko, L. F., Борисенко, Λ. Φ. (1967) Trace elements in pyroxenes and amphiboles from ultramafic rocks of the Urals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 403-410 doi:10.1180/minmag.1967.036.279.10
Plain TextBorisenko, L. F., Борисенко, Λ. Φ. (1967) Trace elements in pyroxenes and amphiboles from ultramafic rocks of the Urals. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 403-410 doi:10.1180/minmag.1967.036.279.10
In(1966) Mineralogical Magazine Vol. 36 (279) Mineralogical Society
Abstract/NotesSummaryThe minor elements Li, Sc, V, Cr, Co, Ni, Ga, Rb, and Sr have been determined in a number of diopsides and horneblendes from ultramafic rocks of the Gussevogorsk, Baranchinsk, and Nizhne-Tagilsk massifs in the Urals. Actinolite and anthophyllite are rare contact metamorphic products ; they too were analysed. The diopside and hornblende from the earlier-formed rocks, richer in olivine, contain more Cr and less V and Ti than those from the later-formed rocks.


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