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Fayalite-bearing high-silica rhyolite eruption at Mono Craters

Name: Fayalite-bearing high-silica rhyolite eruption at Mono Craters
Location: Mono Craters during the mid-Holocene With ~30 high-silica rhyolite domes and flows and a total eruptive volume of ~5??"8.5 km3(DRE)

Mono Craters during the mid-Holocene With ~30 high-silica rhyolite domes and flows and a total eruptive volume of ~5??"8.5 km3(DRE)

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Stanford-hosted lecture on mid-Holocene effusive eruptions at the Mono Craters, focusing on fayalite-bearing high-silica rhyolite, mineralogy changes and 238U-230Th ion-microprobe dating; free to attend.

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Tagsvolcanology geochronology Mono Craters rhyolite ion-microprobe

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