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Analytical method: INAA

TechniqueINAA
MaterialWHOLE ROCK
Mineralnone
InstitutionLOS ALAMOS NATIONAL LABORATORY, EARTH SCIENCE DIVISION, LOS ALAMOS, NM 87545, USA
ReferenceBroxton, David E; Warren, Richard G; Byers, Frank M, Jr; Scott, Robert B (1989) Chemical and mineralogic trends within the Timber Mountain-Oasis Valley caldera complex, Nevada; evidence for multiple cycles of chemical evolution in a long-lived silicic magma system. Journal of Geophysical Research, B, Solid Earth and Planets, vol.94, no.5, pp.5961-5985, 10 May 1989

Samples analysed with this method

Older Tuffs Unit C, Older Tuffs Unit A, Lithic Ridge Tuff, Crater Flat Tuff -Tram Member, Crater Flat Tuff - Bullfrog Member, Stockade Wash Tuff, Crater Flat Tuff - Prow Pass Member, Mafic-rich units of Tuffs and Lavas of Area 20, Mafic-poor units of Tuffs and Lavas of Area 20, Paintbrush Tuff - Rhyolite of Topopah Spring Member, Paintbrush Tuff - Quartz Latite of Topopah Spring Member, Pre-Pah Canyon rhyolite, Paintbrush Tuff - Pah Canyon Member, Px-bearing rhyolite lava, Hb-bearing Rhyolite lava, Paintbrush Tuff - Yucca Mountain member, Paintbrush Tuff - Tiva Canyon member Rhyolite, Paintbrush Tuff - Tiva Canyon member Quartz Latite, Bt-Bearing Rhyolite Lava, Qtz- Bearing Rhyolite Lava, Rhyolite Lavas of Windy Wash, Pre-Ranier Mesa Lavas, Paintbrush Tuff - Ranier Mesa Member - Rhyolite, Paintbrush Tuff - Ranier Mesa Member - Quartz Latite, Pre-Ammonia Tanks Rhyolite Lava, Timber Mountain Tuff - Ammonia Tanks Member - Rhyolite, Timber Mountain Tuff - Ammonia Tanks Member - Quartz Latite, Tuffs of Fleur-de-lis Ranch, Rhyolite of Beatty Wash