Palaeomagnetism and KAr age of Mesozoic and Cenozoic igneous rocks from Antarctica

A new analysis of palaeomagnetic data for igneous rocks from Deception Island, 25 de Mayo Island (King George Island) and Cape Spring, are given. K-Ar age determinations indicate that most of the igneous samples from 25 de Mayo Island included in the palaeomagnetic study are of Late Mesozoic/Early T...

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Autor principal: Valencio, D.A
Otros Autores: Mendía, JosE, Vilas, J.F
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 1979
Acceso en línea:Registro en Scopus
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100 1 |a Valencio, D.A. 
245 1 0 |a Palaeomagnetism and KAr age of Mesozoic and Cenozoic igneous rocks from Antarctica 
260 |c 1979 
270 1 0 |m Valencio, D.A.; Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales ; Ciudad Universitaria, Pabellón 2, Buenos Aires, Argentina 
506 |2 openaire  |e Política editorial 
504 |a Valencio, Fourcade, Estudio paleomagnético y petrográfico de algunas formaciones cenozoicas de las Islas Shetland del Sur (1969) Contrib. Inst. Antárt. Argentino, 125, p. 25 
504 |a Codignotto, Lorente, Mendía, Olivero, Spikerman, Geología del Cabo Spring e islas Pingüino, César y Leopardo (1978) Contrib. Inst. Antárt. Argentino, 216, p. 41 
504 |a Hawkes, The geology of the South Shetland Islands, II. The geology and petrology of Deception Island, Falkland Islands Dependencies (1961) Br. Antarct. Surv., Sci. Rep., 27 
504 |a Olsacher, Contribución a la Geología de la Isla Decepción de la Antártida Occidental (1956) Publ. Inst. Antárt. Argentino, 2. , Parte I 
504 |a Blundell, Palaeomagnetic investigations in the Falkland Island Dependencies (1962) Br. Antarct. Surv., Sci. Rep., 39, p. 24 
504 |a Schauer, Fourcade, Geological-petrographical study of western end of 25 de Mayo Island (King George Island), South Shetland Islands (1963) SCAR Proc., , Cape Town, Antarctic Geology 
504 |a Orlando, The fossil flora of the surroundings of Ardley Peninsula, 25 de Mayo Island, South Shetland Islands (1964) Antarctic Geology, pp. 629-636. , R.J. Adie, North-Holland, Amsterdam 
504 |a Dalziel, Elliot, Evolution of the Scotia Arc (1971) Nature, 233, pp. 246-252 
504 |a Llorente, Mendía, Spikerman, Geología del extremo occidental del Cabo Spring, Costa de Danco, Antártida Argentina (1974) Contrib. Inst. Antárt. Argentino, 173 
504 |a Fisher, Dispersion on a sphere (1953) Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 217, pp. 295-305. , Ser. A 
504 |a Wilson, Dagley, McCormak, Palaeomagnetic evidence about the source of the geomagnetic field (1972) Geophysical Journal International, 28, pp. 213-224 
504 |a McElhinny, Embleton, Wellman, A synthesis of Australian Cenozoic palaeomagnetic results (1974) Geophysical Journal International, 36, pp. 141-151 
504 |a Dalziel, Lowrie, Kligfield, Opdyke, Palaeomagnetic data form the southernmost Andes and the Antarctandes (1973) Implications of Continental Drift to the Earth Sciences, 1, pp. 87-101. , Academic Press, London 
504 |a Hamilton, Formation of the Scotia and Caribbean Arcs (1966) Geol. Surv. Can. Paper 66-15, pp. 178-187 
504 |a Kellogg, Reynolds, Palaeomagnetic results from the Lassiter Coast Antarctica and a test of oroclinal bending of the Antarctic Peninsula (1978) Journal of Geophysical Research, 83, pp. 2293-2299 
504 |a Turnbull, Some palaeomagnetic measurements in Atarctica (1953) Artic, 12, pp. 151-157 
504 |a McElhinny, Embleton, Australian paleomagnetism and the Phanerozoic plate tectonics of eastern Gondwanaland (1974) Tectonophysics, 22, pp. 1-29 
504 |a Vilas, Valencio, Palaeogeographic reconstructions of the Gondwanic continents based on palaeomagnetic and sea-floor spreading data (1970) Earth Planet. Sci. Lett., 7, pp. 397-405 
520 3 |a A new analysis of palaeomagnetic data for igneous rocks from Deception Island, 25 de Mayo Island (King George Island) and Cape Spring, are given. K-Ar age determinations indicate that most of the igneous samples from 25 de Mayo Island included in the palaeomagnetic study are of Late Mesozoic/Early Tertiary age. The significance of these palaeomagnetic-radiometric data on the hypothesis of oroclinal bending of the Antarctic Peninsula and on the apparent polar movement of Antarctica is discussed. The positions of palaeomagnetic poles for the Andean igneous complex indicate that there has not been any apparent post-Late Cretaceous/Early Tertiary oroclinal bending in the Antarctic Peninsula from 74°S to 62°S. A comparison of the positions of palaeomagnetic poles for Antarctica and Australia suggests that the direction of apparent polar movement relative to Antarctica reversed after the Miocene. © 1979.  |l eng 
536 |a Detalles de la financiación: The authors wish to thank the Instatuto AntfirtlcO Argentlno, The Umversldad de Buenos Ages and the Consejo Naclonal de lnvestlgaclones Caentfficas y T6cmcas for the support whach enabled the work described to be carned out 
593 |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales ; Ciudad Universitaria, Pabellón 2, Buenos Aires, Argentina 
593 |a Consejo Nacional de Investigaciones Cientificas y Técnicas, Rivadavia, 1917 Buenos Aires, Argentina 
593 |a Servicio Geológico Nacional, Santa Fe, 1548, Argentina 
690 1 0 |a CAPE SPRING 
690 1 0 |a DECEPTION ISLAND 
690 1 0 |a KING GEORGE ISLAND 
690 1 0 |a OROCLINAL BENDING 
690 1 0 |a POLAR MOVEMENTIGNEOUS ROCKS 
700 1 |a Mendía, JosE. 
700 1 |a Vilas, J.F. 
773 0 |d 1979  |g v. 45  |h pp. 61-68  |k n. 1  |p Earth Plan. Sci. Lett.  |x 0012821X  |w (AR-BaUEN)CENRE-4446  |t Earth and Planetary Science Letters 
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