Palaeomagnetic data from Late Glacial glaciolacustrine sediments at Rio Corintos, Chubut, Argentina

The characteristics of the Pleistocene glaciations in Patagonia have been partially solved. On the basis of the moraine extent and the varve-counting method, and by analogy with the Weichselian Glaciation in Scandinavia, Caldenius (1932) established a pattern of Patagonian glaciations which has rema...

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Autor principal: Beraza, L.A
Otros Autores: Vilas, J.F.A
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 1990
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024 7 |2 scopus  |a 2-s2.0-0025659544 
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100 1 |a Beraza, L.A. 
245 1 0 |a Palaeomagnetic data from Late Glacial glaciolacustrine sediments at Rio Corintos, Chubut, Argentina 
260 |c 1990 
270 1 0 |m Beraza, L.A.; Laboratorio de Paleomagnetismo Daniel A. Valencio, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon 11, 1428 Buenos Aires, Argentina 
506 |2 openaire  |e Política editorial 
504 |a Auer, The Pleistocene of Fuego-Patagonia (1956) Part I. The Ice and Interglacial Ages, 45, p. 226. , III Geologica-Geographica, Ann. Acad. Sci. Fennicae, Helsinki 
504 |a Barton, McElhinny, A 10,000 years geomagnetic secular variation record for three Australian maars (1981) Geophys. J.R. Astron. Soc., 67, pp. 465-485 
504 |a Caldenius, Las glaciaciones cuaternarias en la Patagonia y Tierra del Fuego. (1932) Dir. Gen. de Minas y Geología, (95), p. 152 
504 |a Constable, McElhinny, Holocene geomagnetic secular variation records from northeastern Australian lake sediments (1985) Geophysical Journal International, 81, pp. 103-120 
504 |a Creer, Tucholka, Secular variations as recorded in lake sediments a discussion of N American and European results (1982) Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 306, pp. 87-102 
504 |a Creer, Tucholka, Construction of type curves of geomagnetic secular variation for dating lake sediments from east-central North America (1982) Can. J. Earth Sci., 19, pp. 1106-1115 
504 |a Creer, Tucholka, On the current state of lake sediments paleomagnetic research (1983) Geophys. J.R. Astron. Soc., 74, pp. 223-238 
504 |a Creer, Anderson, Lewis, Late Quaternary geomagnetic stratigraphy recorded in Lake Erie sediments (1976) Earth Planet Sci. Lett., 31, pp. 37-47 
504 |a Creer, Hogg, Readman, Reynaud, Paleomagnetic secular variation curves extending back to 13,400 years BP recorded by sediments deposited in Lac de Joux, Switzerland (1980) J. Geophys., 48, pp. 139-147 
504 |a Creer, Readman, Papamarinopoulos, Geomagnetic secular variation in Greece through the last 6,000 years obtained from lake sediments studies (1981) Geophys. J.R. Astron. Soc., 66, pp. 193-219 
504 |a Creer, Valencio, Sinito, Tucholka, Vilas, Geomagnetic secular variations 0–14,000 years BP as recorded by lake sediments from Argentina (1983) Geophys. J.R. Astron. Soc., 74, pp. 199-222 
504 |a Creer, Smith, Tucholka, Bonifay, Thouveny, Truze, A preliminary paleomagnetic study of the Holocene and late Würmian sediments of Lac du Bouchet (Haute-Loire, France) (1986) Geophys. J.R. Astron. Soc., 86, pp. 943-964 
504 |a Flint, Fidalgo, Geología glacial de la zona de borde entre los paralelos 39 ° 10′ y 41 ° 20′ de latitud sur en la Cordillera de los Andes, República Argentina (1963) Dir. Nac. de Geología y Minería, (93), p. 20 
504 |a Flint, Fidalgo, (1968) Drift glacial al este de los Andes entre Bariloche y Esquel, p. 18. , Instituto Nacional de Geología y Minería, No. 119 
504 |a Kodama, Rabassa, Evenson, Clinch, Paleomagnetismo y edad relativa del Drift Pichileufú en su área tipo, San Carlos de Bariloche, Rio Negro (1986) Asoc. Geol. Arg. Rev., 41 (1-2), pp. 165-178 
504 |a Mercer, Glacial history of southermost South America (1976) Quat. Res. (N.Y.), 6, pp. 125-166 
504 |a Nabel, Valencio, La magnetoestratigrafia del Ensenadense de la ciudad de Buenos Aires: su significado geológico (1981) Asoc. Geol. Arg. Rev., 36 (1), pp. 7-18 
504 |a Sylwan, Paleomagnetic record of a sequence of Late Glacial varves at Lago Buenos Aires, Patagonia, Argentina (1987) International Union of Geodesy and Geophysics XIX General Assembly, 2 v, p. 474. , Vancouver, Abstr 
504 |a Turner, Thompson, Lake sediment record of the geomagnetic secular variation in Britain during Holocene times (1981) Geophys. J.R. Astron. Soc., 65, pp. 703-725 
504 |a Vilas, Equipo para la desmagnetización de rocas para el estudio paleomagnético de las mismas (1966) Thesis, , Dep. Ciencias Fisicas, Universidad de Buenos Aires, (unpublished) 
504 |a Vilas, El magnetómetro UBA 8 Hz y su aplicación en los estudios paleomagnéticos (1979) Doctoral Thesis, , Dep. Ciencias Fisicas, Universidad de Buenos Aires, (unpublished) 
520 3 |a The characteristics of the Pleistocene glaciations in Patagonia have been partially solved. On the basis of the moraine extent and the varve-counting method, and by analogy with the Weichselian Glaciation in Scandinavia, Caldenius (1932) established a pattern of Patagonian glaciations which has remained acceptable. Palaeomagnetic studies of glacial sediments have been started with the aim of testing this correlation. A 78-m Late Glacial glaciolacustrine sequence was studied and sampled at Rio Corintos, Chubut Province, Argentina (43 ° 10′ S, 71 ° 15′ W). Approximately 1089 varves were counted; they were thought to have been deposited between 25 000-13 000 years BP. The samples showed strong and stable values of remanent magnetization. Magnetite was identified as the carrier of the remanence. Magnetic susceptibility and intensity were recorded and the expected variations according to grain size were obtained. Recorded declination values oscillated from 30 ° W to 15 ° E, and inclination values from -8 ° to - 56 °. This shift can be attributed to the secular variation of the geomagnetic field. Declination and inclination values were smoothed using a stratigraphic window which covered 40 varves. Assuming that a single varve implies that one year has passed, the secular variation curve can be presented against a scale-time which spans approximately 1200 years. The corresponding VGP path showed 100% clockwise motion in the region of northern Canada. A correlation with other VGPs recorded in Lago Buenos Aires for Late Glacial varves has been established. © 1990.  |l eng 
593 |a Laboratorio de Paleomagnetismo Daniel A. Valencio, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon 11, 1428 Buenos Aires, Argentina 
690 1 0 |a GLACIOLACUSTRINE SEDIMENT 
690 1 0 |a LATE GLACIAL 
690 1 0 |a LATE GLACIAL SEDIMENT 
690 1 0 |a MORAINE 
690 1 0 |a PALAEOMAGNETIC DATA 
690 1 0 |a PALAEOMAGNETISM 
690 1 0 |a VARVE 
651 4 |a ARGENTINA, CHUBUT, RIO CORINTOS 
700 1 |a Vilas, J.F.A. 
773 0 |d 1990  |g v. 64  |h pp. 111-120  |k n. 2-4  |p Phys. Earth Planet. Inter.  |x 00319201  |w (AR-BaUEN)CENRE-18  |t Physics of the Earth and Planetary Interiors 
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856 4 0 |u https://doi.org/10.1016/0031-9201(90)90031-R  |y DOI 
856 4 0 |u https://hdl.handle.net/20.500.12110/paper_00319201_v64_n2-4_p111_Beraza  |y Handle 
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