| Registros del 1 al 10 de 18 encontrados |
1.- Arc-continent collision and orocline formation; closing of the Central American Seaway
American Geophysical Union; Washington, DC; USA; United States, 2012
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2.- Assessing reference conditions and physico-chemical status according to the European Water Framework Directive; a case-study from the Basque Country (northern Spain)
Elsevier; Oxford; GBR; United Kingdom, 2005
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3.- Caribbean affinities of mafic crust from northern Colombia; preliminary geochemical results from basaltic rocks of the Sinu-San Jacinto Belt
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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4.- Channel incision in the Rio Atenguillo, Jalisco, Mexico, defined by (super 36) Cl measurements of bedrock
Elsevier; Amsterdam; NLD; Netherlands, 2010
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5.- CLIMATOLOGICAL COUPLING OF THE THERMOHALINE DECADAL CHANGES IN CENTRAL WATER OF THE EASTERN NORTH ATLANTIC
2000
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6.- Evidence for middle Eocene and younger land emergence in central Panama; implications for isthmus closure
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
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7.- From arc-continent collision to continuous convergence, clues from Paleogene conglomerates along the southern Caribbean-South America plate boundary
Elsevier; Amsterdam; NLD; Netherlands, 2012
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8.- GEOCHEMISTRY AND GEOCHRONOLOGY OF THE GUAJIRA ECLOGITES, NORTHERN COLOMBIA: EVIDENCE OF A METAMORPHOSED PRIMITIVE CRETACEOUS CARIBBEAN ISLAND-ARC
2011
SUBDUCTION ZONES OF THE CARIBBEAN: THE SEDIMENTARY, MAGMATIC, METAMORPHIC AND ORE-DEPOSIT RECORDS (UNESCO/IUGS IGCP PROJECT 546)
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9.- Incorporation of island-arc rocks into a Caribbean subduction channel; geochemical constraints from eclogite boulders and greenschist rocks, Guajira region, Colombia
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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10.- Integrated provenance studies in northwestern South America; linking tectonic and sedimentary processes
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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