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contourite
Can deepwater bottom currents generate clinothems? An example of a large, asymmetric mounded drift in Upper Jurassic to Lower Cretaceous sediments from northwestern Australia
Late Miocene−Quaternary seismic stratigraphic responses to tectonic and climatic changes at the northeastern margin of the South China Sea
Ichnofabric analysis as a tool for characterization and differentiation between calcareous contourites and calciturbidites
The Nazca Drift System – palaeoceanographic significance of a giant sleeping on the SE Pacific Ocean floor
Inherited morphobathymetric controls over contourite drift deposition: A case study from the late Cenozoic Mentelle Basin, Australia
High-resolution acoustic data revealing periplatform sedimentary characteristics in the Xisha Archipelago, South China Sea
Echofacies interpretation of Pleistocene to Holocene contourites on the Demerara Plateau and abyssal plain
Multistage unidirectionally migrating canyons and the evolution of their trajectories in the canyon zone in the Baiyun Sag, northern South China Sea: Insights into canyon genesis
Late Miocene contourite channel system reveals intermittent overflow behavior
Deep-water channel morphologies, architectures, and population densities in relation to stacking trajectories and climate states
Cannibalism of contourites by gravity flows: explanation of the facies distribution of the Ordovician Pingliang Formation along the southern margin of the Ordos Basin, China
Miocene start of modern carbonate platforms
Cenozoic Contourites in the Eastern Great Australian Bight, Offshore Southern Australia: Implications For the Onset of the Leeuwin Current
Characterization of the natural fracture system of the Eagle Ford Formation (Val Verde County, Texas)
Hybrid turbidite–contourite systems of the Tanzanian margin
Abstract The inversion of a sedimentary basin could be associated with compressional reactivation of basin-forming normal faults, upwards movement of the basement blocks and partial or complete erosion of its sedimentary infill. Basin inversion might be also related to whole-basin uplift that is not linked to the reactivation of basement faults, and results in the development of regional stratigraphic gaps and unconformities. Both types of basin inversion have been documented in SE Poland using seismic data. Regional NW–SE seismic profiles illustrate earliest Late Jurassic (earliest Oxfordian) and earliest Late Cretaceous (Cenomanian) regional unconformities related to regional basin-scale uplifts in the SE segment of the Polish Basin. Late Cretaceous (Turonian?–Maastrichtian) progressive uplift of the Mid-Polish Swell has been documented along the NE border zone of this regional anticlinal structure. The Upper Cretaceous inversion-related sedimentary succession is characterized by an overall progradational character directed from the SW towards the NE. Buried contourite drifts that were detected within the Upper Cretaceous succession using seismic data indicate the existence of contour currents encircling inversion-related intrabasinal morphological barriers. A new tectonic scenario of the Mesozoic evolution of SE Poland would have a significant impact on the modelling of tectonic subsidence and the history of petroleum systems.
Carbonate slope morphology revealing a giant submarine canyon (Little Bahama Bank, Bahamas)
Large bedforms on contourite terraces: Sedimentary and conceptual implications
Vigorous deep-sea currents cause global anomaly in sediment accumulation in the Southern Ocean
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.