Registros del 1 al 10 de 15 encontrados |
![](./images/clear.gif) 1.- Cenozoic provenance history of synorogenic conglomerates in western Argentina (Famatina Belt); implications for central Andean foreland development
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
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![](./images/clear.gif) 2.- Clay mineralogy and thermal history of the Neogene Vinchina Basin, Central Andes of Argentina; analysis of factors controlling the heating conditions
American Geophysical Union; Washington, DC; USA; United States, 2011
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![](./images/clear.gif) 3.- Dynamic topography in South America
Elsevier; Oxford; GBR; United Kingdom, 2013
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![](./images/clear.gif) 4.- Dynamics of deformation and sedimentation in the northern Sierras Pampeanas; an integrated study of the Neogene Fiambala Basin, NW Argentina; discussion
Geological Society of America (GSA); Boulder, CO; USA; United States, 2010
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![](./images/clear.gif) 5.- EARLY MIDDLE MIOCENE BROKEN FORELAND DEVELOPMENT IN THE SOUTHERN CENTRAL ANDES; EVIDENCE FOR EXTENSION PRIOR TO REGIONAL SHORTENING
BLACKWELL SCIENCE; OXFORD; GBR; UNITED KINGDOM, 2003
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![](./images/clear.gif) 6.- Evolution of the landforms across which the Atacama Desert is draped, 20 degrees -24 degrees S latitude
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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![](./images/clear.gif) 7.- Exhumation history of the Andean broken foreland revisited
Geological Society of America (GSA); Boulder, CO; USA; United States, 2013
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![](./images/clear.gif) 8.- Magnetostratigraphy and paleomagnetism of early and middle Miocene synorogenic strata; basement partitioning and minor block rotation in Argentine broken foreland
Springer International; Berlin; DEU; Germany, 2011
Multi-accretional tectonics at the Rio de la Plata Craton margins
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![](./images/clear.gif) 9.- Miocene forebulge development previous to broken foreland partitioning in the southern Central Andes, west-central Argentina
American Geophysical Union; Washington, DC; USA; United States, 2007
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![](./images/clear.gif) 10.- ORDOVICIAN BACK ARC FORELAND AND OCLOYIC THRUST BELT DEVELOPMENT ON THE WESTERN GONDWANA MARGIN AS A RESPONSE TO PRECORDILLERA TERRANE ACCRETION
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
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