Crustal shortening, exhumation, and strain localization in a collisional orogen: The Bajo Pequeño Shear Zone, Sierra de Pie de Palo, Argentina-Reference-Cited by-同舟云学术

Crustal shortening, exhumation, and strain localization in a collisional orogen: The Bajo Pequeño Shear Zone, Sierra de Pie de Palo, Argentina

Published:2014-07 Issue:7 Volume:33 Page:1277-1303
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Garber Joshua M.¹²,Roeske Sarah M.¹,Warren Jessica³,Mulcahy Sean R.⁴,McClelland William C.⁵,Austin Lauren J.⁶,Renne Paul R.⁴⁷,Vujovich Graciela I.⁸⁹

Affiliation:

1. Department of Geology; University of California; Davis California USA

2. Now at Department of Earth Science; University of California; Santa Barbara California USA

3. Department of Geological and Environmental Sciences; Stanford University; Stanford California USA

4. Department of Earth and Planetary Science; University of California; Berkeley California USA

5. Department of Geoscience; University of Iowa; Iowa City Iowa USA

6. Department of Geological Sciences; University of Oregon; Eugene Oregon USA

7. Berkeley Geochronology Center; Berkeley California USA

8. CONICET; Buenos Aires Argentina

9. Laboratorio de Tectonica Andina-FCEyN; Universidad de Buenos Aires; Buenos Aires Argentina

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference90 articles.

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3. Abundances of the elements; meteoritic and solar;Anders;Geochim. Cosmochim. Acta,1989

4. The early Paleozoic evolution of the Argentine Precordillera as a Laurentian rifted, drifted, and collided terrane: A geodynamic model;Astini;Geol. Soc. Am. Bull.,1995

5. Austin , L. J. S. M. Roeske J. M. Garber J. Winpenny Q. Yin 2011 Detrital zircon geochronology of lower to mid-crustal rocks associated with a microplate-continent collision

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