El volcanismo cuaternario en el retroarco de Payenia: una revisión
EJ Llambías, GW Bertotto, C Risso… - Revista de la …, 2010 - SciELO Argentina
La provincia basáltica Payenia se desarrolló al pie de los Andes entre 33º40'S y 38ºS. Es
una típica asociación de retroarco con dos picos de actividad, el más antiguo es …
una típica asociación de retroarco con dos picos de actividad, el más antiguo es …
[HTML][HTML] Monogenetic basaltic volcanoes: genetic classification, growth, geomorphology and degradation
G Kereszturi, K Németh - Updates in volcanology-new advances in …, 2012 - intechopen.com
Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …
Payenia volcanic province in the Southern Andes: An appraisal of an exceptional Quaternary tectonic setting
VA Ramos, A Folguera - Journal of Volcanology and geothermal Research, 2011 - Elsevier
The Southern Volcanic Zone of the Andes has a Quaternary basaltic province along the
retroarc which has a unique tectonic setting. The Payenia volcanic province covers an area …
retroarc which has a unique tectonic setting. The Payenia volcanic province covers an area …
Retroarc volcanism in the northern San Rafael Block (34–35 30′ S), southern Central Andes: Occurrence, age, and tectonic setting
A Folguera, JA Naranjo, Y Orihashi, H Sumino… - Journal of Volcanology …, 2009 - Elsevier
One of the major retroarc volcanic provinces in the southern Central Andes (34° and 37° S)
is developed in the Andean foothills of the San Rafael region between the orogenic front …
is developed in the Andean foothills of the San Rafael region between the orogenic front …
Geomorphometric variability of “monogenetic” volcanic cones: evidence from Mauna Kea, Lanzarote and experimental cones
M Kervyn, GGJ Ernst, JC Carracedo, P Jacobs - Geomorphology, 2012 - Elsevier
Volcanic cones are the most common volcanic constructs on Earth. Their shape can be
quantified using two morphometric ratios: the crater/cone base ratio (Wcr/Wco) and the cone …
quantified using two morphometric ratios: the crater/cone base ratio (Wcr/Wco) and the cone …
Payenia volcanic province, southern Mendoza, Argentina: OIB mantle upwelling in a backarc environment
N Søager, PM Holm, EJ Llambías - Chemical Geology, 2013 - Elsevier
The Pleistocene to Holocene Payenia volcanic province is a backarc region of 60,000 km2
in Mendoza, Argentina, which is dominated by transitional to alkaline basalts and …
in Mendoza, Argentina, which is dominated by transitional to alkaline basalts and …
The intra-continental Al Madinah Volcanic Field, Western Saudi Arabia: a proposal to establish Harrat Al Madinah as the first volcanic geopark in the Kingdom of Saudi …
MR Moufti, K Németh - Geoheritage, 2013 - Springer
Abstract The United Nations Educational, Scientific and Cultural Organization promotes
conservation of geological and geomorphological heritage through the promotion and …
conservation of geological and geomorphological heritage through the promotion and …
Olivine major and trace element compositions in southern Payenia basalts, Argentina: evidence for pyroxenite–peridotite melt mixing in a back-arc setting
Olivine major and trace element compositions from 12 basalts from the southern Payenia
volcanic province in Argentina have been analyzed by electron microprobe and laser …
volcanic province in Argentina have been analyzed by electron microprobe and laser …
Volcanic evolution of the back-arc Pleistocene Payun Matru volcanic field (Argentina)
For the first time, about 30 volcanic formations of the back-arc Payun Matru volcanic field
(Payun Matru volcanic field, Argentina, 36° S, 69° W) have been sampled for K–Ar …
(Payun Matru volcanic field, Argentina, 36° S, 69° W) have been sampled for K–Ar …
Morphological and statistical characterisation of recent mafic volcanism on Tenerife (Canary Islands, Spain)
Tenerife is the largest island of the Canarian Archipelago and presents a complex volcanic
history. The construction of a mafic shield and a phonolitic composite volcano represent the …
history. The construction of a mafic shield and a phonolitic composite volcano represent the …