Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica
Deception Island is an active volcano with a large structural collapse that has been interpreted by several investigators as having been generated by different processes. The general stratigraphy and structural study of the volcano is presented, with special emphasis on the distribution and structur...
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Elsevier Ltd
2000
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| LEADER | 14131caa a22010337a 4500 | ||
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| 001 | PAPER-2148 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250910090920.0 | ||
| 008 | 190411s2000 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0034464945 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Baraldo, A. | |
| 245 | 1 | 0 | |a Stratigraphy and structure of Deception Island, South Shetland Islands, Antarctica |
| 260 | |b Elsevier Ltd |c 2000 | ||
| 270 | 1 | 0 | |m Baraldo, A.; Departamento de Geologia, Universidad de Buenos Aires, Pabellon II Ciudad Universitaria, Buenos Aires 1428, Argentina; email: andres@gl.fcen.uba.ar |
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| 504 | |a Hawkes, D.D., The geology of the South Shetlands, I: The geology and petrology of Deception Island (1961) Falkland Island Dependencies Survey, Scientific Report, 27, pp. 1-43 | ||
| 504 | |a Hoteldahl, O., On the geology and physiography of some Antarctic and Subantarctic islands (1929) Scientifics Results of the Norwegian Antarctic Expedition, 1927-1928, 1, pp. 98-99 | ||
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| 504 | |a Mazzuoli, R., Omarini, R.H., Ortiz-Ramis, R., Viramonte, J.G., De Rosa, R., Mecanismos eruptivos de la actividad explosiva reciente en la Isla Decepción, Shetland del Sur, Antártida (1987) X Congreso Geológico Argentino, 4, pp. 378-379. , Actas | ||
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| 504 | |a Orheim, O., Volcanic activity on Deception Island (1971) Antarctic Geology and Geophysics, pp. 117-120. , Adie, R.J. (Ed.), Universitetsforlaget, Oslo, Norway | ||
| 504 | |a Ortiz, R., Diez-Gil, J.L., Viramonte, J.G., Modelo para la simulación del transporte y depositación de piroclastos. Aplicación al estudio de las erupciones de 1967, 1969 y 1970, ocurridos en Decepción (Antártida) (1987) XXI Reunión Bienal, p. 4648. , Real Sociedad Espan̄ola de Física (4-10 Octubre. 1987, Madrid) | ||
| 504 | |a Ortiz, R., Vila, J., García, A., Camacho, A.G., Diez, J.L., Aparicio, A., Soto, R., Petrinovic, I., Geophysical features of Deception Island (1992) Recent Progress in Antarctic Earth Science, pp. 443-448. , Yoshida, Y., et al. (Eds.) | ||
| 504 | |a Parra, J.C., González Ferrán, O., Bannister, J., Aeromagnetic survey over the South Shetland Islands. Bransfield Strait and part of the Antarctic Peninsula (1984) Revista Geológica De Chile, 23, pp. 3-20 | ||
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| 504 | |a Risso, C., Caselli, A., Aparicio, A., Ortiz, R., (1994) Nuevos Aspectos Petrológicos De La Isla Decepción Antártida, 3, pp. 201-215. , Servicio de Publicaciones Cabildo Insular de Lanzarote (España), Serie Casa de los Volcanes | ||
| 504 | |a Roobol, M.J., Historic volcanic activity at Deception Island (1973) British Antarctic Survey Bulletin, 32, pp. 23-30 | ||
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| 504 | |a Weaver, S.D., Saunders, A., Pankhurst, R.J., Tarney, J., A geochemical study of magmatism associated with the initial stages of back-arc spreading: The Quaternary volcanics of Bransfield from South Shetland Islands (1979) Contributions in Mineralogy and Petrology, 64, pp. 151-169 | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a Deception Island is an active volcano with a large structural collapse that has been interpreted by several investigators as having been generated by different processes. The general stratigraphy and structural study of the volcano is presented, with special emphasis on the distribution and structural disposition of the different stratigraphic units. The rocks of Deception Island have traditionally been divided into pre- and post-caldera products. A subdivision of the pre-caldera deposits, called 'pre- and syn-caldera deposits,' has been observed in two main units. Bulk magnetic susceptibility analyses are used to support the field stratigraphy presented. The localization and distribution of dikes is used to assign the central collapse of the volcano to rifting induced by tensional tectonics occurring in the Bransfield Strait and the presence of transcurrent faults around the island. © 2000 Elsevier Science Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: The authors would like to thank the following people for their assistance during 1996 and 1997: Dra. C. Risso and the staff of the Volcanologic Observatory on Deception Island (Instituto Antártico Argentino, Consejo Superior de Investigaciones Cientı́ficas de España); the crew of the Deception Island Argentine Station; and R.E.T. Gabriel de Castilla (Spain). We are grateful to Dr A. Rapalini for his direction in the paleomagnetic analyses, which were carried out at the Daniel Valencio Paleomagnetism Laboratory, University of Buenos Aires. Thanks also to Drs M. Remesal, F. Salani, and J. Viramonte for their critical reviews of this paper. An internal fellowship from CONICET to A. Baraldo supported this research. | ||
| 593 | |a Departamento De Geología, Universidad De Buenos Aires, Pabellón II Ciudad Universitaria, 1428 Buenos Aires, Argentina | ||
| 593 | |a CONICET, Instituto Antártico Argentino, Argentina | ||
| 690 | 1 | 0 | |a ANTARCTICA |
| 690 | 1 | 0 | |a DECEPTION ISLAND |
| 690 | 1 | 0 | |a VOLCANIC CALDERAS |
| 690 | 1 | 0 | |a VOLCANOES |
| 690 | 1 | 0 | |a CALDERA |
| 690 | 1 | 0 | |a STRATIGRAPHY |
| 690 | 1 | 0 | |a STRUCTURAL GEOLOGY |
| 690 | 1 | 0 | |a VOLCANO |
| 690 | 1 | 0 | |a ANTARCTICA |
| 690 | 1 | 0 | |a DECEPTION ISLAND |
| 690 | 1 | 0 | |a SOUTH SHETLAND ISLANDS |
| 700 | 1 | |a Rinaldi, Carlos Alberto | |
| 773 | 0 | |d Elsevier Ltd, 2000 |g v. 13 |h pp. 785-796 |k n. 8 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
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