Prehistoric to historic volcanic activity at Copahue volcano
Copahue is one of the most active volcanic centers in Argentina. Despite the relatively intense volcanic activity its prehistoric events are poorly known. In this work, after a brief introduction on the geological and structural control on this volcanic complex, we have summarized the events that ha...
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Springer Berlin Heidelberg
2015
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| LEADER | 09307caa a22007337a 4500 | ||
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| 001 | PAPER-13253 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518204333.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84956552702 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Caselli, A.T. | |
| 245 | 1 | 0 | |a Prehistoric to historic volcanic activity at Copahue volcano |
| 260 | |b Springer Berlin Heidelberg |c 2015 | ||
| 270 | 1 | 0 | |m Caselli, A.T.; LESVA, IIPG, Universidad Nacional de Río Negro, Roca 1242, Argentina; email: atcaselli@unrn.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Delpino, D., Bermudez, A., La actividad volcánica del volcán Copahue durante 1992. Erupción con emisión de azufre piroclástico. Provincia de Neuquén (1993) XII Congreso Geológico Argentino, 4, pp. 292-301. , Mendoza | ||
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| 504 | |a Folguera, A., Ramos, V., Control estructural del volcán Copahue (38°S-71°O): implicancias tectónicas para el arco volcánico cuaternario (36-39° S) (2000) Rev Asoc Geol Arg, 55 (3), pp. 229-244 | ||
| 504 | |a Folguera, A., Ramos, V.A., Melnick, D., Recurrencia en el desarrollo de cuencas de intra-arco. Cordillera Neuquina (37°30′) (2003) Rev Asoc Geol Arg, 58, pp. 3-19 | ||
| 504 | |a Frequent ash explosions and acidic mudflows starting on July 1 (2000) Glob Volcano Netw Bull, 25 | ||
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| 504 | |a Groeber, P., La región de Copahue y su glaciación diluvial (1921) Rev Soc Arg Estudios Geográficos, 1, pp. 92-110 | ||
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| 504 | |a Lowell, T.V., Heusser, C.J., Andersen, B.G., Moreno, P.I., Hauser, A., Heusser, L.E., Schlüchter, C., Denton, G.H., Interhemispheric correlation of late pleistocene glacial events (1995) Science, 269, pp. 1541-1549 | ||
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| 504 | |a Petit-Breuilh, M.E., Cronología eruptiva histórica de los volcanes Planchón-Peteróa y Copahue, Andes del sur (1996) Proyecto de Riesgo volcánico, p. 45. , Servicio Nacional de Geología y Minería, Santiago, Chile | ||
| 504 | |a Polanco, E., (2003) Evolución del volcán Copahue (37 45'S), Andes del Sur, p. 90. , Tesis de Maestría (Unpublished), Instituto de Geofísica, Universidad Autónoma de México, México | ||
| 504 | |a Polanco, E., Naranjo, J.A., Young, S., Moreno, H., Volcanismo Explosivo Holoceno en la cuenca del alto Bio-Bio, Andes del Sur (37 45′-38 30′ S) (2000) IX Congreso Geológico Chileno, Puerto Varas, Chile, 2, pp. 59-61 | ||
| 504 | |a Sepúlveda, M.E., La historia eruptiva de los volcanes hispanoamericanos (siglos XVI al XX). Servicio de Publicaciones del Exmo (2004) Cabildo Insular de Lanzarote-Casa de los volcanes, p. 431 | ||
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| 504 | |a Varekamp, J.C., Ouimette, A.P., Herman, S.W., Bermúdez, A., Delpino, D., Hydrothermal element fluxes from Copahue, Argentina: a "beehive" volcano in turmoil (2001) Geology, 29, pp. 1059-1062 | ||
| 504 | |a Varekamp, J.C., Maarten deMoor, J., Merrill, M., Colvin, A., Goss, A., Vroon, P., Hilton, D., Geochemistry and isotopic characteristics of Caviahue-Copahue volcanic complex, Province of Neuquen, Argentina (2006) Geol Soc Am Special Paper, 407, pp. 317-342. , En Kay S, y Ramos A (eds) Evolution of an Andean margin: a tectonic and magmatic view from the Andes to the Neuquen Basin (35°-39°S lat) | ||
| 504 | |a Watt, S., Pyle, D., Mather, T., The influence of great earthquakes on volcanic eruption rate along the Chilean subduction zone (2009) Earth Planet Sci Lett, 277, pp. 399-407 | ||
| 520 | 3 | |a Copahue is one of the most active volcanic centers in Argentina. Despite the relatively intense volcanic activity its prehistoric events are poorly known. In this work, after a brief introduction on the geological and structural control on this volcanic complex, we have summarized the events that have led to the construction of the current volcanic edifice and its historical eruptive activity. Prehistoric events were divided into three main stages: pre-, sin- and post-glacial based on the stratigraphic relations observed in the field by previous authors. At least 13 eruptions were recorded during the last 260 years. Although the scarce detailed historical information, the eruptive style outlined by the available reports and data seems to indicate a general phreatic and phreato-magmatic character over the last two centuries, whereas the most recent (2000 and 2012) eruptive events, characterized by the occurrence of magmatic pulses, have a strombolian character. © Springer-Verlag Berlin Heidelberg 2016. All rights are reserved. |l eng | |
| 593 | |a LESVA, IIPG, Universidad Nacional de Río Negro, Roca 1242, General Roca, 8332, Argentina | ||
| 593 | |a Dpto. Cs. Geológicas, FCEN, Universidad de Buenos Aires, 1428 Ciudad Universitaria, Pab.2, Buenos Aires, Argentina | ||
| 593 | |a CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina | ||
| 593 | |a Department of Earth Sciences, University of Florence, Via La Pira 4, Florence, 50121, Italy | ||
| 700 | 1 | |a Velez, M.L. | |
| 700 | 1 | |a Agusto, M. | |
| 700 | 1 | |a Liccioli, C. | |
| 700 | 1 | |a Vaselli, O. | |
| 773 | 0 | |d Springer Berlin Heidelberg, 2015 |h pp. 49-59 |p Copahue Volcano |z 9783662480052 |z 9783662480045 |w (AR-BaUEN)BIBLO-48631 |t Copahue Volcano | |
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