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Garnet within Qbt. Rick Warren and Fraser Goff Retired, Los Alamos National Laboratory. Thin sections for SWNVF. Garnet habits in volcanics. SWNVF : GT in 60 of 313 thin sections JVF : GT in 10 of 76 thin sections. Grain shown is largest found, .091 mm (91,000 square microns).
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Garnet within Qbt Rick Warren and Fraser Goff Retired, Los Alamos National Laboratory
Garnet habits in volcanics SWNVF: GT in 60 of 313 thin sections JVF: GT in 10 of 76 thin sections Grain shown is largest found, .091 mm (91,000 square microns)
Garnet areas in thin section SWNVF only 131 grains
Stratigraphic units and lithologies • All stratigraphic assemblages for SWNVF • From base to top of Qbt for JVF • Fractions of each lithology for SWNVF: • 62% are nonwelded tuff • 15% are welded tuff • 12% are alluvia • 7% are vitrophyric tuff • 3% are rhyolite lava
Origin of garnet in volcanics • Necklaces require pneumatolytic origin • Carbonates completely absent • Argillites can provide Ca, Fe for andradite • Andradite also forms in other host lithics • Almandines likely detrital • Prevalence in SWNVF suggests that pneumatolytic andradite/grossular may commonly form in rhyolite vents