Pre-Eruptive Conditions of the Oligocene Wah Wah Springs Tuff, Southeastern Great Basin Ignimbrite Province
The Wah Wah Springs Tuff (30.0 Ma) is one of several very large volume ash-flow tuffs (>3200 km³ of erupted magma) that were emplaced near the peak of the flare-up of activity in the Great Basin ignimbrite province of western North America. It can be characterized as a "monotonous intermedia...
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| Format: | Others |
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BYU ScholarsArchive
2008
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| Online Access: | https://scholarsarchive.byu.edu/etd/1568 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=2567&context=etd |