High-temperature, large-volume, lavalike ash-flow tuffs without calderas in southwestern Idaho stratigraphy and petrology of rhyolites that were erupted as ash flows from depths too great to allow the development of calderas and at such high temperatures that the ash flows coalesced to form liquids before final emplacement and cooling
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| Weitere Verfasser: | , |
| Format: | UnknownFormat |
| Sprache: | eng |
| Veröffentlicht: |
Washington, DC
U.S. Gov. Print. Off.
1984
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| Schriftenreihe: | Geological Survey professional paper / United States Department of the Interior
1272 |
| Schlagworte: |
Owyhee County, Idaho
> Vulkanasche
> Aschentuff
> Stratigraphie
> Gesteinskunde
> Geochemie
> Idaho
> Neogen
> Quartär
> Rhyolith
> Tuff
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Tag hinzufügen | Beschreibung: | IV, 76 S. Ill., graph. Darst., Kt. 2 Kt.-Beil. |
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