Registros del 1 al 8 de 8 encontrados |
![](./images/clear.gif) 1.- An investigation of lithospheric structure and evolution in convergent orogenic systems using seismic receiver functions and surface wave analysis
2008
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![](./images/clear.gif) 2.- BAJA ALASKA/BRITISH COLUMBIA AND BAJA CALIFORNIA; SEPARATED TWINS?
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
GEOLOGICAL SOCIETY OF AMERICA, 1998 ANNUAL MEETING
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![](./images/clear.gif) 3.- Catastrophic glacial multi-phase mass movements; a special type of glacial hazard
European Geosciences Union; Katlenburg-Lindau; III; International, 2008
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![](./images/clear.gif) 4.- EVIDENCE FROM GARIBALDI PROVINCIAL PARK, BRITISH COLUMBIA, FOR A COMPLEX HISTORY OF HOLOCENE GLACIER FLUCTUATIONS IN THE WESTERN CORDILLERA OF THE AMERICAS
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2004
GEOLOGICAL SOCIETY OF AMERICA, 2004 ANNUAL MEETING
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![](./images/clear.gif) 5.- Paleobiogeographic patterns along western North America and constraints of terrane transport scenarios
Geological Association of Canada; Waterloo, ON; CAN; Canada, 2003
Geological Association of Canada, Mineralogical Association of Canada; joint annual meeting; abstracts--Association geologique du Canada, Association mineralogique du Canada; congres annuel conjointe; recueil des resumes
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![](./images/clear.gif) 6.- Tectonic vs. magmatic processes and the anatomy of Andean arcs
Elsevier; New York, NY; III; International, 2006
Abstracts of the 16th annual V. M. Goldschmidt conference
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![](./images/clear.gif) 7.- The Kaniksu and Idaho Batholiths, northern U.S. Cordillera; close relatives or a case of mistaken identity?
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
Geological Society of America, 2012 annual meeting
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![](./images/clear.gif) 8.- Thermal history of the Ecstall, and Butedale Plutons; (super 40) Ar/ (super 39) Ar thermochronology and thermal modeling
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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