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Abstract:

The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks that were penetratively deformed during Ordovician accretion of the Precordillera terrane to the Gondwana margin. New structural, petrologic, and geochronologic data from a 40 km structural transect reveals that the Sierra de Pie de Palo preserves a middle to lower crustal ductile thrust complex consisting of individual structural units and not an intact ophiolite and cover sequence. Top-to-the-west thrusting occurred intermittently on discrete ductile shear zones from ∼515 to ∼417 Ma and generally propagated toward the foreland with progressive deformation. Ordovician crustal shortening and peak metamorphic temperatures in the central portion of the Sierra de Pie de Palo were synchronous with retro-arc shortening and magmatic flare-up within the Famatina arc. Accretion of the Precordillera terrane resulted in the end of arc flare-up and the onset of synconvergent extension by ∼439 Ma. Continued synextensional to postextensional convergence was accommodated along progressively lower grade shear zones following terrane accretion and the establishment of a new plate margin west of the Precordillera terrane. The results support models of Cordilleran orogens that link voluminous arc magmatism to periods of regional shortening. The deformation, metamorphic, and magmatic history within the Sierra de Pie de Palo is consistent with models placing the region adjacent to the Famatina margin in the middle Cambrian and not as basement to the Precordillera terrane. Copyright 2011 by the American Geophysical Union.

Registro:

Documento: Artículo
Título:Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
Autor:Mulcahy, S.R.; Roeske, S.M.; McClelland, W.C.; Jourdan, F.; Iriondo, A.; Renne, P.R.; Vervoort, J.D.; Vujovich, G.I.
Filiación:Department of Geoscience, University of Nevada, Las Vegas, Las Vegas, NV, United States
Department of Earth and Planetary Sciences, University of California, Berkeley, CA 94720-4767, United States
Department of Geology, University of California, Davis, CA 95616, United States
Department of Geoscience, University of Iowa, Iowa City, IA 52242, United States
Western Australian Argon Isotope Facility, Department of Applied Geology and JdLCMS, Curtin University of Technology, Perth, WA 6845, Australia
Berkeley Geochronology Center, Berkeley, CA 94709, United States
Centro de Geociencias, Universidad Nacional Autónoma de México, Campus Juriquilla, Querétaro, 76230, Mexico
Department of Earth and Planetary Science, University of California, Berkeley, CA, United States
School of Earth and Environmental Sciences, Washington State University, Pullman, WA 99164, United States
Department of Geology, University of Buenos Aires-CONICET, Ciudad Universitaria, C1428EHA Buenos Aires, Argentina
Palabras clave:Deformation; Stratigraphy; Tectonics; Arc magmatism; Cambrians; Crustal shortening; Ductile shear zone; Ductile thrusts; Northwest Argentina; Ordovician; Orogens; Progressive deformation; Shear zone; Structural evolution; Structural unit; Synconvergent extension; Terrane accretion; Metamorphic rocks; accretion; Cambrian; crustal shortening; deformation; geochronology; Gondwana; Ordovician; orogeny; petrology; shear zone; structural geology; tectonic evolution; terrane; Argentina; Precordillera
Año:2011
Volumen:30
Número:1
DOI: http://dx.doi.org/10.1029/2009TC002656
Título revista:Tectonics
Título revista abreviado:Tectonics
ISSN:02787407
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02787407_v30_n1_p_Mulcahy

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Citas:

---------- APA ----------
Mulcahy, S.R., Roeske, S.M., McClelland, W.C., Jourdan, F., Iriondo, A., Renne, P.R., Vervoort, J.D.,..., Vujovich, G.I. (2011) . Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina. Tectonics, 30(1).
http://dx.doi.org/10.1029/2009TC002656
---------- CHICAGO ----------
Mulcahy, S.R., Roeske, S.M., McClelland, W.C., Jourdan, F., Iriondo, A., Renne, P.R., et al. "Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina" . Tectonics 30, no. 1 (2011).
http://dx.doi.org/10.1029/2009TC002656
---------- MLA ----------
Mulcahy, S.R., Roeske, S.M., McClelland, W.C., Jourdan, F., Iriondo, A., Renne, P.R., et al. "Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina" . Tectonics, vol. 30, no. 1, 2011.
http://dx.doi.org/10.1029/2009TC002656
---------- VANCOUVER ----------
Mulcahy, S.R., Roeske, S.M., McClelland, W.C., Jourdan, F., Iriondo, A., Renne, P.R., et al. Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina. Tectonics. 2011;30(1).
http://dx.doi.org/10.1029/2009TC002656