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High fluorine rhyolite; an eruptive pegmatite magma at the Honeycomb Hills, Utah.

Congdon, Roger D; Nash, W P (1988) High fluorine rhyolite; an eruptive pegmatite magma at the Honeycomb Hills, Utah. Geology Boulder. 16; 11, Pages 1018-1021. 1988.

AuthorsCongdon, Roger D; Nash, W P
Year1988
TitleHigh fluorine rhyolite; an eruptive pegmatite magma at the Honeycomb Hills, Utah.
SourceGeology Boulder. 16; 11, Pages 1018-1021. 1988.
PublisherGeological Society of America GSA. Boulder, CO, United States. 1988.
Document typeSerial
ISSN0091-7613
GeoRef1988-076266
Keywordsacidic-magmas; chemical-composition; composition-; fluorine-; genesis-; geochemistry-; granitic-composition; halogens-; Honeycomb-Hills; igneous-rocks; Juab-County-Utah; lava-; magma-chambers; magmas-; metals-; partitioning-; pegmatitic-composition; phenocrysts-; rare-earths; rhyolites-; trace-elements; United-States; Utah-; viscosity-; volcanic-rocks; west-central-Utah
DOI10.1130/0091-7613(1988)016<1018:HFRAEP>2.3.CO;2

4 samples from this reference

SampleRock nameMajorTraceIsotope
PumiceRhyolite yesyes
Vitrophyre Whole RockRhyolite yesyes
Vitrophyre GlassRhyolite yesyes
DomeRhyolite yesyes