Crustal motion in the Southern Andes (26°-36°S): Do the Andes behave like a microplate?-Reference-Cited by-同舟云学术

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Crustal motion in the Southern Andes (26°-36°S): Do the Andes behave like a microplate?

Published:2003-10 Issue:10 Volume:4 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Brooks Benjamin A.¹,Bevis Michael¹,Smalley Robert²,Kendrick Eric¹,Manceda René³,Lauría Eduardo⁴,Maturana Rodrigo⁵,Araujo Mario⁶

Affiliation:

1. School of Ocean and Earth Science and Technology; University of Hawaii; 1680 East-West Road, Honolulu Hawaii 96822 USA

2. Center for Earthquake Research and Information; University of Memphis; 3876 Central Ave Ste 1, Memphis Tennessee 38152 USA

3. RepsolYPF; 1330 Lake Robbins Drive, The Woodlands Texas 77380 USA

4. Instituto Geográfico Militar Argentina; Cabildo 381, Buenos Aires Argentina

5. Instituto Geográfico Militar Chile; Dieciocho N° 369, Santiago Chile

6. Instituto Nacional de Prevención Sísmica; Roger Balet Norte 47, 5400 San Juan Argentina

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference45 articles.

1. Foreland shortening and crustal balancing in the Andes at 30°S latitude;Allmendinger;Tectonics,1990

2. Space-geodetic estimation of the Nazca-South America Euler vector;Angermann;Earth Planet. Sci. Lett.,1999

3. Spatial distribution of earthquakes and subduction of the Nazca plate beneath South America;Barazangi;Geology,1976

4. Crustal deformation during 1994-1998 due to oblique continental collision in the central Southern Alps, New Zealand, and implications for seismic potential of the Alpine Fault;Beavan;J. Geophys. Res.,1999

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