Ekren, E. B., & McIntyre, D. H. (1984). 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. United States Gov. Print. Off.
Chicago-Zitierstil (17. Ausg.)Ekren, Einar B., und David H. McIntyre. 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. Washington: United States Gov. Print. Off, 1984.
MLA-Zitierstil (9. Ausg.)Ekren, Einar B., und David H. McIntyre. 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. United States Gov. Print. Off, 1984.