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research vessels
On the Possibility of Developing a Seismoelectrical Method for Direct Hydrocarbon Prospecting in the Arctic Seas without the Use of a Streamer Cable
Stratigraphic Drilling in the Northern Kara Sea: First Case and Preliminary Results
Possibilities of River Seismic Survey for Studying the Structure of the Earth’s Crust and the Upper Mantle of the Territory of Siberia
Enhanced weathering in the seabed: Rapid olivine dissolution and iron sulfide formation in submarine volcanic ash
The continent-to-ocean transition in the Iberia Abyssal Plain
Impact of bending-related faulting and oceanic-plate topography on slab hydration and intermediate-depth seismicity
The First Data on the Mineralogy and Geochemistry of the Suspension of Lake Onego
Methane Fluxes at the Water–Atmosphere Interface and Gas-Geochemical Anomalies in the Bottom Sediments in the Northwestern Part of the Sea of Japan
Molecular Geochemistry of the Dispersed Organic Matter in the Late Cenozoic Sediments of the Laptev Sea Continental Margin and Adjacent Part of the Arctic Ocean
Hydrocarbon Molecular Markers as Indicators of the Late Cenozoic Sedimentation on the Amerasian Continental Margin (Arctic Ocean)
Chemical Composition and Genesis of Ferromanganese Crusts from the Sonne Ridge (Kuril Basin, Sea of Okhotsk)
The geological work of the Scottish National Antarctic Expedition, 1902 – 04
DARWIN THE GEOLOGIST IN SOUTHERN SOUTH AMERICA
Structure of the Demerara passive-transform margin and associated sedimentary processes. Initial results from the IGUANES cruise
Abstract The IGUANES cruise took place in May 2013 on the R/V L’Atalante along the Demerara passive transform margin off French Guiana and Surinam. Seismic, multibeam and chirp acquisitions were made. Piston cores were collected for pore geochemistry and sedimentology. A mooring was deployed on the sea-bottom for 10 months (temperature, salinity, turbidity and current measurements). This new dataset highlights the lateral variability of the 350 km-long Guiana–Surinam transform margin due to the presence of a releasing bend between two transform segments. The adjacent Demerara Plateau is affected by a 350 km-long giant slide complex. This complex initiated in Cretaceous times and was regularly reactivated until recent times. Since the Miocene, contourite processes seem to be active due to the onset of the North Atlantic Deep Water (NADW) bottom current. A main NADW water vein flows towards SE, eroding slide headscarps and allowing the deposition of contourite drifts. Numerous depressions looking like comet tails or comet scours record this flow. Some of those were interpreted before the cruise as active pockmarks. Pore geochemistry and core analysis do not show any evidence of present-day gas seepage.