| Registros del 1 al 5 de 5 encontrados |
1.- CHILE TRIPLE JUNCTION AREA; DACITIC MAGMATISM OVER A SUBDUCTING ACTIVE SPREADING RIDGE, CHARACTERIZATION AND ORIGIN
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000
AGU 2000 FALL MEETING
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2.- CONTINENTAL MARGIN STRUCTURE AND EVOLUTION CONTROLLED BY RIDGE SUBDUCTION (CHILE TRIPLE JUNCTION AREA, 46-47 DEGREES S)
[INTERNATIONAL GEOLOGICAL CONGRESS]; [LOCATION VARIES]; III; INTERNATIONAL, 2000
BRAZIL 2000; 31ST INTERNATIONAL GEOLOGICAL CONGRESS; ABSTRACTS VOLUME
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3.- NEW SR, ND AND O ISOTOPIC COMPOSITION OF RIDGE-SUBDUCTION RELATED LAVAS (TAITAO PENINSULA, CHILE TRIPLE JUNCTION AREA)
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1997
AGU 1997 FALL MEETING
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4.- Subduction of the south Chile active spreading ridge; a 17 Ma to 3 Ma magmatic record in central Patagonia (western edge of Meseta del Lago Buenos Aires, Argentina)
Elsevier; Amsterdam; NLD; Netherlands, 2010
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5.- TWO PHASES OF OPHIOLITE EMPLACEMENT AT THE CHILE MARGIN TRIPLE JUNCTION AREA (46-47S)
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1999
AGU 1999 FALL MEETING
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