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Abstract:

Early Paleozoic paleomagnetic data from NW Argentina and Northern Chile have shown large systematic rotations within two domains: one composed of the Western Puna that yields very large (up to 80°) counter-clockwise rotations, and the other formed by the Famatina Ranges and the Eastern Puna that shows (~40°) clockwise rotations around vertical axes. In several locations, lack of significant rotations in younger rocks constrains this kinematic pattern to have occurred during the Paleozoic. Previous tectonic models have explained these rotations as indicative of rigid-body rotations of large para-autochthonous crustal blocks or terranes. A different but simple tectonic model that accounts for this pattern is presented in which rotations are associated to crustal shortening and tectonic escape due to the collision of the allochthonous terrane of Precordillera in the Late Ordovician. This collision should have generated dextral shear zones in the back arc region of the convergent SW Gondwana margin, where systematic domino-like clockwise rotations of small crustal blocks accommodate crustal shortening. The Western Puna block, bordering the Precordillera terrane to the north, might have rotated counterclockwise as an independent microplate due to tectonic escape processes, in a fashion similar to the present-day relationship between the Anatolia block and the Arabian microplate. © 2010 Springer-Verlag.

Registro:

Documento: Artículo
Título:Reinterpretation of the Ordovician rotations in NW Argentina and Northern Chile: A consequence of the Precordillera collision?
Autor:Spagnuolo, C.M.; Rapalini, A.E.; Astini, R.A.
Filiación:IESGLO, Instituto de Sedimentología, Fundación Miguel Lillo, Miguel Lillo 251, T4000JFE San Miguel de Tucumán, Argentina
INGEODAV, Depto. Cs. Geológicas, FCEyN, Univ. Buenos Aires, Ciudad Universitaria, Pabellón 2, C1428EHA Buenos Aires, Argentina
Laboratorio de Análisis de Cuencas, CICTERRA, CONICET-UNC, Avenida Vélez Sársfield 1611, X5016GCA Córdoba, Argentina
Palabras clave:Block rotations; Gondwana; NW Argentina; Paleomagnetism; Paleozoic; block rotation; collision zone; crustal shortening; kinematics; microplate; Ordovician; paleomagnetism; Paleozoic; shear zone; Anatolia; Argentina; Chile; La Rioja [Argentina]; Sierra de Famatina; Sierras Pampeanas; Turkey
Año:2011
Volumen:100
Número:2
Página de inicio:603
Página de fin:618
DOI: http://dx.doi.org/10.1007/s00531-010-0578-2
Título revista:International Journal of Earth Sciences
Título revista abreviado:Int. J. Earth Sci.
ISSN:14373254
CODEN:IJESF
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_14373254_v100_n2_p603_Spagnuolo

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Citas:

---------- APA ----------
Spagnuolo, C.M., Rapalini, A.E. & Astini, R.A. (2011) . Reinterpretation of the Ordovician rotations in NW Argentina and Northern Chile: A consequence of the Precordillera collision?. International Journal of Earth Sciences, 100(2), 603-618.
http://dx.doi.org/10.1007/s00531-010-0578-2
---------- CHICAGO ----------
Spagnuolo, C.M., Rapalini, A.E., Astini, R.A. "Reinterpretation of the Ordovician rotations in NW Argentina and Northern Chile: A consequence of the Precordillera collision?" . International Journal of Earth Sciences 100, no. 2 (2011) : 603-618.
http://dx.doi.org/10.1007/s00531-010-0578-2
---------- MLA ----------
Spagnuolo, C.M., Rapalini, A.E., Astini, R.A. "Reinterpretation of the Ordovician rotations in NW Argentina and Northern Chile: A consequence of the Precordillera collision?" . International Journal of Earth Sciences, vol. 100, no. 2, 2011, pp. 603-618.
http://dx.doi.org/10.1007/s00531-010-0578-2
---------- VANCOUVER ----------
Spagnuolo, C.M., Rapalini, A.E., Astini, R.A. Reinterpretation of the Ordovician rotations in NW Argentina and Northern Chile: A consequence of the Precordillera collision?. Int. J. Earth Sci. 2011;100(2):603-618.
http://dx.doi.org/10.1007/s00531-010-0578-2