ARE TITANITE GRAINS IN MIDDLE AND LATE JURASSIC TUFFS OF THE CARMEL AND MORRISON FORMATIONS OF UTAH VOLCANIC IN ORIGIN OR DETRITAL GRAINS FROM NON-VOLCANIC SOURCES? | Zendy

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ARE TITANITE GRAINS IN MIDDLE AND LATE JURASSIC TUFFS OF THE CARMEL AND MORRISON FORMATIONS OF UTAH VOLCANIC IN ORIGIN OR DETRITAL GRAINS FROM NON-VOLCANIC SOURCES?

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