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Rio Grande Rise
Vulnerable Marine Ecosystems – Processes and Practices in the High Seas Vulnerable Marine Ecosystems Processes and Practices in the High Seas
20. a Seismic Reflection Study of the Rio Grande Rise1
The Geodynamic Development of the Rio Grande Rise and Walvis Ridge, Central South Atlantic Ocean, from Crustal Thickness Mapping
Rio Grande Rise Hot Spot System' Implicationsfor African and South American Plate Motions Over Plumes
End of a Modern Geological Myth: There Are No Rudists in Brazil! Paleobiogeographic Implications
Crustal Thickness Mapping of the Central South Atlantic and The
New Developments Regarding the KT Event and Other Catastrophes in Earth History
Genesis and Evolution of Ferromanganese Crusts from the Summit of Rio Grande Rise, Southwest Atlantic Ocean
OCN 201 Mantle Plumes and Hot Spots
A Review of Pangaea Dispersal and Large Igneous Provinces – in Search of a T Causative Mechanism ⁎ Alexander L
Geostrophic Velocity Measurement Techniques for the Meridional Overturning Circulation and Meridional Heat Transport in the South Atlantic
A Biophysical Profile of the Tristan Da Cunha Archipelago (PDF)
Characterization of the Rio Grande Rise from Elements of the Terrestrial Gravity Field
Commission on the Limits of the Continental Shelf
Tectonic Forcings of Maastrichtian Ocean-Climate Evolution
Major Intensification of Atlantic Overturning Circulation at the Onset
South Atlantic Paleobathymetry Since Early Cretaceous Lucía Pérez-Díaz 1 & Graeme Eagles2
2. Regional Oceanographic Setting of the Southwestern Atlantic1
Top View
Deep Sea Drilling Project Initial Reports Volume 72
51. Tectonic Evolution and Subsidence History of the Rio Grande Rise1
Southeastern Atlantic Deep-Water Evolution During the Late-Middle Eocene to Earliest Oligocene (Ocean Drilling Program Site 1263 and GEOSPHERE; V
How and When Plume Zonation Appeared During the 132&Thinsp
A German Contribution to South Atlantic Seabed Studies, 1938-39 by Colin Summerhayes1 and Cornelia Lüdecke2
THE Official Magazine of the OCEANOGRAPHY SOCIETY
Large Igneous Provinces: Crustal Structure, Dimensions, and External Consequences
Tectonically Restricted Deep-Ocean Circulation at the End of the Cretaceous Greenhouse
Submerged Archipelago