| Registros del 1 al 10 de 26 encontrados |
1.- Andean adakite-like high-Mg andesites on the northern margin of the Chilean-Pampean flat-slab (27-28.5 degrees S) associated with frontal arc migration and fore-arc subduction erosion
Oxford University Press; Oxford; GBR; United Kingdom, 2013
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2.- Cenozoic tectonics and porphyry copper systems of the Chilean Andes
Society of Economic Geologists; Littleton, CO; USA; United States, 2012
Geology and genesis of major copper deposits and districts of the world; a tribute to Richard H. Sillitoe
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3.- CENTRAL ANDEAN ORE DEPOSITS LINKED TO EVOLVING SHALLOW SUBDUCTION SYSTEMS AND THICKENING CRUST
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
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4.- CLOCKWISE BLOCK ROTATIONS ALONG THE EASTERN BORDER OF THE CORDILLERA DE DOMEYKO, NORTHERN CHILE (22 DEGREES 45'-23 DEGREES 30'S)
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2000
ADVANCES IN PALEOMAGNETISM AND TECTONICS OF ACTIVE MARGINS; IN HONOR OF RETIREMENT OF MYRL E. BECK, JR.
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5.- Continental underthrusting and obduction during the Cretaceous closure of the Rocas Verdes rift basin, Cordillera Darwin, Patagonian Andes
American Geophysical Union; Washington, DC; USA; United States, 2010
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6.- EL SALVADOR PORPHYRY COPPER SYSTEM, CHILE; A MAGMATIC RESPONSE TO THE MIDDLE EOCENE INCAIC DEFORMATION PHASE
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2000
GEOLOGICAL SOCIETY OF AMERICA, CORDILLERAN SECTION AND ASSOCIATED SOCIETIES, 96TH ANNUAL MEETING; ABSTRACTS
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7.- EL SALVADOR, CHILE PORPHYRY COPPER DEPOSIT REVISITED; GEOLOGIC AND GEOCHRONOLOGIC FRAMEWORK
WINSTON & SON; SILVER SPRING, MD; USA; UNITED STATES, 1997
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8.- EOCENE TO EARLY PLIOCENE GEOLOGY OF THE CHILE'S EL INDIO GOLD DISTRICT
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2000
GEOLOGICAL SOCIETY OF AMERICA, CORDILLERAN SECTION AND ASSOCIATED SOCIETIES, 96TH ANNUAL MEETING; ABSTRACTS
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9.- EPISODIC MAGMATIC FRONT MIGRATION AND MOUNTAIN BUILDING PROCESSES IN THE CENTRAL ANDES OF NORTHERN CHILE; THE LAST 180 MA
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2003
GEOLOGICAL SOCIETY OF AMERICA, 2003 ANNUAL MEETING
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10.- 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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