Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina
Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic ter...
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2004
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| LEADER | 16200caa a22012737a 4500 | ||
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| 001 | PAPER-21089 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205231.0 | ||
| 008 | 190411s2004 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-10644284912 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Vizán, H. | |
| 245 | 1 | 0 | |a Paleomagnetism of Upper Triassic rocks in the Los Colorados hill section, Mendoza province, Argentina |
| 260 | |c 2004 | ||
| 270 | 1 | 0 | |m Vizán, H.; CONICET, Departamento de Ciencias Geologicas, Universidad de Buenos Aires, Pabellón 2, Buenos Aires 1428, Argentina; email: haroldo@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Different authors have highlighted a systematic disagreement between Late Carboniferous-Triassic paleomagnetic poles (PPs) for Gondwanaland and Laurasia when they are repositioned in a classical reconstruction prior to the breakup of Pangea A. This disagreement has been interpreted in geodynamic terms or as an evidence of non-dipole components of the geomagnetic field. Such analyses have been made using data on South American PPs published approximately 25 years ago and obtained using outdated methodologies. In this article, the authors present new Late Triassic paleomagnetic data from rocks that crop out in the Pre-Andean ranges (Precordillera) of Mendoza province (Argentina). Samples of different lithologies were taken from two limbs of a doubly plunging syncline, and several field tests of paleomagnetic stability were applied. The results indicate primary site mean directions that yield a PP with geographic coordinates and statistical parameters as follows: Lat.=76°S, Lon.=280°E, N=12, R=11.63, α95=8°, K=30.2. This PP agrees with mean PPs of Laurasia of similar ages in different models of Pangea A, indicating that the hypothesis of a dipolar paleomagnetic field could be valid for the Late Triassic. © 2004 Elsevier Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: University of Birmingham | ||
| 536 | |a Detalles de la financiación: We thank the Universidad de Buenos Aires, the University of Birmingham and CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas) for financial support of the research. Dr J. Genise helped us during the fieldwork. Special thanks to Drs R. Somoza, S.E. Geuna, C. Marcicano (U.B.A.) for help with a revision of a prevous version of this paper. H.V. is in debt to the research staff of the ‘old'School of Earth Sciences of the University of Birmingham. The careful reviews by Drs D. Tarling and A. Rapalini, are appreciated. | ||
| 593 | |a CONICET, Departamento de Ciencias Geologicas, Universidad de Buenos Aires, Pabellón 2, Buenos Aires 1428, Argentina | ||
| 593 | |a School of Earth Sciences, The University of Birmingham, Edgbaston, Birmingham B15 2TT, United Kingdom | ||
| 593 | |a CONICET, Museo Paleontologico Egidio Feruglio, Avenida Fontana 140, 9100 Trelew, Chubut, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a MENDOZA | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a LATE TRIASSIC |
| 690 | 1 | 0 | |a PALEOMAGNETISM |
| 690 | 1 | 0 | |a PANGEA |
| 690 | 1 | 0 | |a PRECORDILLERA |
| 690 | 1 | 0 | |a PALEOMAGNETISM |
| 690 | 1 | 0 | |a PANGAEA |
| 690 | 1 | 0 | |a POLAR WANDERING |
| 690 | 1 | 0 | |a TRIASSIC |
| 690 | 1 | 0 | |a PRECORDILLERA |
| 690 | 1 | 0 | |a WESTERN HEMISPHERE |
| 690 | 1 | 0 | |a WORLD |
| 700 | 1 | |a Ixer, R. | |
| 700 | 1 | |a Turner, P. | |
| 700 | 1 | |a Cortés, J.M. | |
| 700 | 1 | |a Cladera, G. | |
| 773 | 0 | |d 2004 |g v. 18 |h pp. 41-59 |k n. 1 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
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