| Registros del 1 al 10 de 28 encontrados |
1.- A glacially incised canyon in Brazil; further evidence for mid-Ediacaran glaciation?
University of Chicago Press; Chicago, IL; USA; United States, 2013
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2.- A red algal bloom in the aftermath of the Marinoan snowball Earth
Blackwell; Oxford; GBR; United Kingdom, 2007
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3.- Archeointensity in northeast Brazil over the past five centuries
Elsevier; Amsterdam; NLD; Netherlands, 2010
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4.- Carbon and strontium isotope fluctuations and paleoceanographic changes in the late Neoproterozoic Araras carbonate platform, southern Amazon Craton, Brazil
Elsevier; Amsterdam; NLD; Netherlands, 2007
Precambrian chemostratigraphy
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5.- Columbia revisited; paleomagnetic results from the 1790 Ma Colider volcanics (SW Amazonian Craton, Brazil)
Elsevier; Amsterdam; III; International, 2008
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6.- Detrital zircon ages and geochronological constraints on the Neoproterozoic Puga diamictites and associated BIFs in the southern Paraguay Belt, Brazil
Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2013
Ultrahigh pressure and high pressure metamorphic terranes in orogenic belts; reactions, fluids and geological processes
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7.- Direct dating of paleomagnetic results from Precambrian sediments in the Amazon Craton; evidence for Grenvillian emplacement of exotic crust in SE Appalachians of North America
Elsevier; Amsterdam; NLD; Netherlands, 2008
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8.- Direct dating of the Sete Lagoas cap carbonate (Bambui Group, Brazil) and implications for the Neoproterozoic glacial events
Blackwell; Oxford; GBR; United Kingdom, 2007
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9.- G'day Gondwana; the final accretion of a supercontinent; U-Pb ages from the post-orogenic Sao Vicente Granite, northern Paraguay Belt, Brazil
Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2012
Western Gondwana
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10.- GRANITE FABRICS AND REGIONAL-SCALE STRAIN PARTITIONING IN THE SERIDO BELT (BORBOREMA PROVINCE, NE BRAZIL)
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
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