Ordovician back arc foreland and Ocloyic thrust belt development on the western Gondwana margin as a response to Precordillera terrane accretion
- 6 August 2004
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 23 (4)
- https://doi.org/10.1029/2003tc001620
Abstract
No abstract availableKeywords
This publication has 59 references indexed in Scilit:
- “Proterozoic–Early Paleozoic evolution in western South America—a discussion” in: Tectonophysics, 354: 121–137 (2002)Tectonophysics, 2003
- El Grupo Cerro Morado (Ordovícico Medio) en el Famatina (28-29°S), Andes centrales del oeste argentinoRevista geológica de Chile, 2002
- Proterozoic–Early Paleozoic evolution in western South America—a discussionTectonophysics, 2002
- Tracing Crustal Evolution in the Southern Central Andes from Late Precambrian to Permian with Geochemical and Nd and Pb Isotope DataThe Journal of Geology, 2000
- Origin and evolution of the Precordillera terrane of western Argentina: A drifted Laurentian orphanPublished by Geological Society of America ,1999
- Geodynamic evolution and tectonostratigraphic terranes of northwestern Argentina and northern ChileGSA Bulletin, 1997
- Lithospheric modeling of the Ordovician foreland basin in the Puna of northwestern Argentina: on the influence of arc loading on foreland basin formationTectonophysics, 1996
- The early Paleozoic evolution of the Argentine Precordillera as a Laurentian rifted, drifted, and collided terrane: A geodynamic modelGSA Bulletin, 1995
- Foreland basinsGeophysical Journal International, 1981
- Spatial distribution of earthquakes and subduction of the Nazca plate beneath South AmericaGeology, 1976