| Registros del 1 al 8 de 8 encontrados |
1.- A MODERATE TRANSLATION ALTERNATIVE TO THE BAJA BRITISH COLUMBIA HYPOTHESIS
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
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2.- A TRANSPORT STRATIGRAPHY IN THE UPPER CRETACEOUS NANAIMO GROUP, BRITISH COLUMBIA?; THE EVIDENCE AND IMPLICATIONS TO LATE CRETACEOUS LARGE LATITUDINAL TRANSLATION HYPOTHESES
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2003
GEOLOGICAL SOCIETY OF AMERICA, CORDILLERAN SECTION, 99TH ANNUAL MEETING
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3.- COMPARATIVE EVOLUTION OF CRETACEOUS BASINS IN BAJA CALIFORNIA, MEXICO AND BRITISH COLUMBIA; IMPLICATIONS FOR TERRANE TRANSLATION
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
GEOLOGICAL SOCIETY OF AMERICA, 1998 ANNUAL MEETING
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4.- Co-occurring Campanian/Maastrichtian index fossils in the Western Interior and North Pacific biotic provinces require fundamental changes in zonal biostratigraphy for both provinces
Geological Society of America (GSA); Boulder, CO; USA; United States, 2008
Geological Society of America, 2008 annual meeting
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5.- E/I corrected paleolatitudes for the sedimentary rocks of the Baja British Columbia hypothesis
Elsevier; Amsterdam; NLD; Netherlands, 2006
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6.- Integration of macrofossil biostratigraphy and magnetostratigraphy for the Pacific Coast Upper Cretaceous (Campanian-Maastrichtian) of North America and implications for correlation with the Western Interior and Tethys
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
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7.- MEASUREMENTS OF THE CRETACEOUS PALEOLATITUDE OF VANCOUVER ISLAND; CONSISTENT WITH THE BAJA-BRITISH COLUMBIA HYPOTHESIS
AMERICAN ASSOCIATION FOR THE ADVANCEMENT OF SCIENCE; WASHINGTON, DC; USA; UNITED STATES, 1997
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8.- NANAIMO GROUP, SOUTHWEST BRITISH COLUMBIA; A LATE CRETACEOUS BASIN WITH A CONTINUOUS NORTHERN PROVENANCE SIGNATURE
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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