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Kamenetsky, V. S., Morrow, N., McPhie, J. (2000) Origin of high-Si dacite from rhyolitic melt: evidence from melt inclusions in mingled lavas of the 1.6 Ga Gawler Range Volcanics, South Australia. Mineralogy and Petrology, 69 (3) 183-195 doi:10.1007/s007100070020

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Reference TypeJournal (article/letter/editorial)
TitleOrigin of high-Si dacite from rhyolitic melt: evidence from melt inclusions in mingled lavas of the 1.6 Ga Gawler Range Volcanics, South Australia
JournalMineralogy and Petrology
AuthorsKamenetsky, V. S.Author
Morrow, N.Author
McPhie, J.Author
Year2000 (June 26)Volume69
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s007100070020Search in ResearchGate
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Mindat Ref. ID16404Long-form Identifiermindat:1:5:16404:7
GUID0
Full ReferenceKamenetsky, V. S., Morrow, N., McPhie, J. (2000) Origin of high-Si dacite from rhyolitic melt: evidence from melt inclusions in mingled lavas of the 1.6 Ga Gawler Range Volcanics, South Australia. Mineralogy and Petrology, 69 (3) 183-195 doi:10.1007/s007100070020
Plain TextKamenetsky, V. S., Morrow, N., McPhie, J. (2000) Origin of high-Si dacite from rhyolitic melt: evidence from melt inclusions in mingled lavas of the 1.6 Ga Gawler Range Volcanics, South Australia. Mineralogy and Petrology, 69 (3) 183-195 doi:10.1007/s007100070020
In(2000, June) Mineralogy and Petrology Vol. 69 (3) Springer Science and Business Media LLC


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