| Registros del 1 al 3 de 3 encontrados |
1.- CAN THE LATE MIOCENE RAMADAS VOLCANIC CENTRE OF NW ARGENTINA'S ANDEAN PUNA BE CLASSIFIED AS A COLLAPSE CALDERA?
GEOLOGICAL SOCIETY OF AUSTRALIA; SYDNEY, N.S.W.; AUS; AUSTRALIA, 2003
17TH VICTORIAN UNIVERSITIES EARTH SCIENCES CONFERENCE
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2.- EXPLOSIVE PLINIAN ACTIVITY AND DISPERSAL IN THE ANDES; FACIES AND INTERNAL STRATIGRAPHY OF THE LATE MIOCENE CORTE BLANCO TUFF; PUNA PLATEAU, SALTA PROVINCE, NW ARGENTINA
GEOLOGICAL SOCIETY OF AUSTRALIA; SYDNEY, N.S.W.; AUS; AUSTRALIA, 2002
GEOSCIENCE 2002; EXPANDING HORIZONS; ABSTRACTS OF THE 16TH AUSTRALIAN GEOLOGICAL CONVENTION
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3.- The origin of an unusual tuff ring of perlitic rhyolite pyroclasts; the last explosive phase of the Ramadas volcanic centre, Andean Puna, Salta, NW Argentina
Elsevier; Amsterdam; NLD; Netherlands, 2009
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