Registros del 1 al 10 de 12 encontrados |
![](./images/clear.gif) 1.- An early Miocene elasmobranch fauna from the Navidad Formation, central Chile, South America
Backhuys; Leiden; NLD; Netherlands, 2006
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![](./images/clear.gif) 2.- Cenozoic erosion in the Andean forearc in central Chile (33 degrees -34 degrees S); sediment provenance inferred by heavy mineral studies
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
Mineralogical and geochemical approaches to provenance
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![](./images/clear.gif) 3.- Ichnology, sequence stratigraphy and depositional evolution of an Upper Cretaceous rocky shoreline in central Chile; bioerosion structures in a transgressed metamorphic basement
Elsevier;; GBR; United Kingdom, 2011
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![](./images/clear.gif) 4.- Implications of deep-marine Miocene deposits on the evolution of the north Patagonian Andes
University of Chicago Press; Chicago, IL; USA; United States, 2013
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![](./images/clear.gif) 5.- Major forearc subsidence and deep-marine Miocene sedimentation in the present Coastal Cordillera and Longitudinal Depression of south-central Chile (38 degrees 30'S-41 degrees 45'S)
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
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![](./images/clear.gif) 6.- Neogene decapod Crustacea from southern Chile
Carnegie Museum of Natural History; Pittsburgh, PA; USA; United States, 2010
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![](./images/clear.gif) 7.- OSTRACODA FROM MIOCENE DEEP-WATER DEPOSITS IN CENTRAL CHILE; PRELIMINARY RESULTS
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2003
GEOLOGICAL SOCIETY OF AMERICA, 2003 ANNUAL MEETING
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![](./images/clear.gif) 8.- Paleontologic evidence for sedimentary displacement in Neogene forearc basins of central Chile
Society for Sedimentary Geology; Tulsa, OK; USA; United States, 2007
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![](./images/clear.gif) 9.- Rapid and major coastal subsidence during the late Miocene in south-central Chile
Elsevier; Oxford; GBR; United Kingdom, 2008
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![](./images/clear.gif) 10.- Sedimentology, paleontology and age of the Ayacara and Lago Ranco Formations (south-central Chile, 40 degrees -42 degrees S); tectonic implications
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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