Instituto Geológico y Minero de España

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Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 7 de 7 encontrados

1.-  Apatite fission track constraints on the long-term erosional exhumation and landscape evolution of the "Altiplano Antioqueno", Northern Andes, Colombia
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
Geological Society of America, 2007 annual meeting
Ver registro

2.-  Cenozoic exhumation of the Antioqueno Plateau, northern Andes, Colombia, from apatite low-temperature thermochronology
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
Ver registro

3.-  Constraining Cenozoic uplift/exhumation of the Panama-Choco Block by apatite and zircon low-temperature thermochronology; insights on the onset of collision and the morphotectonic history of the region
Geological Society of America (GSA); Boulder, CO; USA; United States, 2010
Geological Society of America, 2010 annual meeting
Ver registro

4.-  Crystallization age and magma sources of the Antioqueno and Ovejas Batholiths, Central Cordillera, Colombia; evidence from combined LA-ICP-MS U/Pb dating and Hf-isotope analysis of zircon grains and whole-rock geochemistry
Geological Society of America (GSA); Boulder, CO; USA; United States, 2009
Geological Society of America, 2009 annual meeting
Ver registro

5.-  Formation age and magma sources for the Antioqueno Batholith derived from LA-ICP-MS uranium-lead dating and hafnium-isotope analysis of zircon grains
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
Geological Society of America, 2007 annual meeting
Ver registro

6.-  Fracturing of the Panamanian isthmus during initial collision with South America
Geological Society of America (GSA); Boulder, CO; USA; United States, 2011
Ver registro

7.-  Long-term erosion and exhumation of the "Altiplano Antioqueno", Northern Andes (Colombia) from apatite (U-Th)/He thermochronology
Elsevier; Amsterdam; NLD; Netherlands, 2009
Ver registro


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