| 词条 | Cerro Beltrán |
| 释义 |
The volcano is located next to the Salar de Antofalla.[2] It is one of the large long-lived volcanoes forming the Archibarca-Galan volcanic alignment, along with Tebenquicho, Galán and Antofalla. References1. ^1 2 {{cite journal|last1=Kraemer|first1=B.|last2=Adelmann|first2=D.|last3=Alten|first3=M.|last4=Schnurr|first4=W.|last5=Erpenstein|first5=K.|last6=Kiefer|first6=E.|last7=van den Bogaard|first7=P.|last8=Görler|first8=K.|title=Incorporation of the Paleogene foreland into the Neogene Puna plateau: The Salar de Antofalla area, NW Argentina|journal=Journal of South American Earth Sciences|date=March 1999|volume=12|issue=2|pages=157–182|doi=10.1016/S0895-9811(99)00012-7|url=http://www.sciencedirect.com/science/article/pii/S0895981199000127|accessdate=22 September 2015}} [1][2]2. ^1 {{cite journal|last1=Cas|first1=Ray A. F.|last2=Wright|first2=Heather M. N.|last3=Folkes|first3=Christopher B.|last4=Lesti|first4=Chiara|last5=Porreca|first5=Massimiliano|last6=Giordano|first6=Guido|last7=Viramonte|first7=Jose G.|title=The flow dynamics of an extremely large volume pyroclastic flow, the 2.08-Ma Cerro Galán Ignimbrite, NW Argentina, and comparison with other flow types|journal=Bulletin of Volcanology|date=16 November 2011|volume=73|issue=10|pages=1583–1609|doi=10.1007/s00445-011-0564-y|issn=1432-0819}} }}{{DEFAULTSORT:Cerro Beltran}}{{Volcanology-stub}} 5 : Miocene volcanoes|Extinct volcanoes|Volcanoes of Argentina|Stratovolcanoes of Argentina|Polygenetic volcanoes |
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