Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Silvina Guzmán"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Externí odkaz:
https://doaj.org/article/a4a832c8e1284683b87c1521e9e77ddf
Publikováno v:
Chemical Geology. 629:121473
Publikováno v:
International Journal of Earth Sciences. 110:2399-2434
Central (18–28° S) and Southern (33–46° S) Andean Volcanic Zones (CVZ and SVZ, respectively) have several Miocene to Recent collapse calderas. We compare their characteristics based on published data to identify how the tectonic variables have
Autor:
Catalina Balbis, C. del Papa, Irene Raquel Hernando, Joaquin Bucher, Jan Oliver Eisermann, Silvina Guzmán, Paul Leon Göllner, Ivan Alejandro Petrinovic
Publikováno v:
International Journal of Earth Sciences. 110:2541-2558
The Caviahue–Copahue volcanic complex in the Southern Volcanic Zone of the Andes is composed of the Pliocene–Pleistocene Caviahue depression and the active Copahue volcano. This volcanic complex is located in a zone of profuse volcanic and tecton
Autor:
Ivan Alejandro Petrinovic, Irene Raquel Hernando, Leandro D'Elia, Silvina Guzmán, Gerardo Nestor Paez
Publikováno v:
Journal of South American Earth Sciences. 90:453-462
The formation of pumice cones by deposition of near-vent pumice fragments is relatively rare in comparison with the occurrence of their mafic equivalents, the scoria cones. The Quaternary Payún Matrú caldera (36° S, 69° W), within the back-arc of
Autor:
Silvina Guzmán, Roberto Carniel
Publikováno v:
Updates in Volcanology-Transdisciplinary Nature of Volcano Science ISBN: 9781838812140
A volcano is a complex system, and the characterization of its state at any given time is not an easy task. Monitoring data can be used to estimate the probability of an unrest and/or an eruption episode. These can include seismic, magnetic, electrom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::45bbb298a6c8899a3ee75dd574d4eb6e
http://hdl.handle.net/11390/1192552
http://hdl.handle.net/11390/1192552
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
We present a detailed stratigraphy of the Coranzulí caldera-forming deposits. This caldera, located in the Altiplano-Puna Volcanic Complex (Central Andes), generated four ignimbrite deposits with similar field characteristics and facies that differ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89f1094471970efe87d536bbb55b69de
http://hdl.handle.net/10261/214127
http://hdl.handle.net/10261/214127
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
instname
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
The Coranzulí caldera (23°00′ S – 66°15′ W) is one of the least known caldera complexes in the eastern part of the Argentinian Altiplano-Puna plateau (Central Andes). It lies at the intersection of N-S, NW-SE and NE-SW fault systems and was
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b2961353229319ab36cc48c63fc4478
http://hdl.handle.net/10261/177262
http://hdl.handle.net/10261/177262
Autor:
Hirochika Sumino, Yuji Orihashi, María Luisa Ochi Ramacciotti, Silvina Guzmán, Florencia Escalante Fochi, Pablo Grosse
Publikováno v:
Journal of Volcanology and Geothermal Research. 401:106966
The back-arc southern Puna region (south of ~24°S) in the Central Volcanic Zone of the Andes contains hundreds of Miocene to Quaternary mafic monogenetic volcanoes roughly distributed in several volcanic fields. Analysis of the geomorphology, morpho
Publikováno v:
Journal of South American Earth Sciences. 62:80-91
New field observations and petrographic and geochemical data of pyroclastic deposits exposed along the Las Papas valley (border between southern Puna and northern Sierras Pampeanas, Argentina) and further north, lead us to propose a new stratigraphic