- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
East Africa
-
Tanzania (1)
-
-
North Africa
-
Morocco (1)
-
-
-
Arctic Ocean (1)
-
Arctic region
-
Greenland
-
West Greenland (1)
-
-
-
Asia
-
Far East
-
Indonesia
-
Sunda Arc (1)
-
-
Japan
-
Honshu
-
Chiba Peninsula (2)
-
-
-
-
-
Atlantic Ocean
-
East Atlantic (1)
-
North Atlantic
-
Faeroe-Shetland Basin (1)
-
Gulf of Cadiz (2)
-
Gulf of Mexico (2)
-
Little Bahama Bank (1)
-
Northeast Atlantic (2)
-
Northwest Atlantic
-
Demerara Rise (1)
-
-
Rockall Plateau (1)
-
Rockall Trough (1)
-
-
South Atlantic
-
Southwest Atlantic (2)
-
-
-
Australasia
-
New Zealand (1)
-
-
Avalon Zone (1)
-
Baffin Bay (1)
-
Canada
-
Eastern Canada
-
Newfoundland and Labrador
-
Newfoundland
-
Avalon Peninsula (1)
-
-
-
-
Mackenzie Mountains (1)
-
Western Canada
-
Northwest Territories (1)
-
-
-
Caribbean region
-
West Indies
-
Bahamas (1)
-
-
-
Europe
-
Southern Europe
-
Iberian Peninsula
-
Portugal (1)
-
-
Italy
-
Apennines (1)
-
Emilia-Romagna Italy
-
Parma Italy (1)
-
-
Marches Italy
-
Pesaro Italy (1)
-
-
Tuscany Italy
-
Pisa Italy (1)
-
Siena Italy (1)
-
-
-
-
Western Europe
-
Scandinavia
-
Denmark (1)
-
-
United Kingdom
-
Great Britain
-
Scotland (1)
-
Wales
-
Welsh Basin (1)
-
-
-
-
-
-
Indian Ocean
-
Mid-Indian Ridge
-
Southeast Indian Ridge (1)
-
-
-
Mediterranean region (1)
-
Mediterranean Sea
-
West Mediterranean (3)
-
-
Mexico
-
Baja California (1)
-
-
North America
-
Great Lakes
-
Lake Superior (1)
-
-
-
Pacific Ocean
-
East Pacific
-
Southeast Pacific (1)
-
-
South Pacific
-
Southeast Pacific (1)
-
-
West Pacific
-
Indonesian Seas (1)
-
-
-
South America
-
Argentina (1)
-
French Guiana (1)
-
Surinam (1)
-
Uruguay (1)
-
-
South Island (1)
-
Southern Ocean (2)
-
Strait of Gibraltar (2)
-
United States
-
Michigan
-
Michigan Upper Peninsula
-
Keweenaw Peninsula (1)
-
-
-
Mississippi River (1)
-
-
-
commodities
-
oil and gas fields (1)
-
petroleum (2)
-
-
elements, isotopes
-
carbon
-
C-14 (2)
-
-
isotope ratios (2)
-
isotopes
-
radioactive isotopes
-
C-14 (2)
-
-
stable isotopes
-
O-18/O-16 (2)
-
-
-
oxygen
-
O-18/O-16 (2)
-
-
-
fossils
-
ichnofossils (1)
-
Invertebrata
-
Protista
-
Foraminifera
-
Rotaliina
-
Globigerinacea
-
Globigerinidae
-
Globigerinoides (1)
-
-
-
-
-
-
-
microfossils (2)
-
palynomorphs
-
Dinoflagellata (1)
-
-
problematic fossils (1)
-
-
geochronology methods
-
paleomagnetism (1)
-
U/Pb (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Holocene
-
upper Holocene (1)
-
-
Kazusa Group (1)
-
Pleistocene
-
upper Pleistocene
-
Weichselian
-
upper Weichselian
-
Younger Dryas (1)
-
-
-
-
-
-
Tertiary
-
Neogene
-
Miocene (2)
-
Pliocene
-
upper Pliocene (1)
-
-
-
Paleogene
-
Eocene (1)
-
Paleocene (1)
-
-
-
-
Laurentide ice sheet (1)
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (2)
-
-
Triassic (2)
-
-
Paleozoic
-
Silurian
-
Lower Silurian
-
Llandovery
-
Aberystwyth Grits (1)
-
-
-
-
-
Precambrian
-
upper Precambrian
-
Proterozoic
-
Neoproterozoic
-
Ediacaran (3)
-
Vendian (2)
-
-
Windermere System (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
volcanic rocks (1)
-
-
-
metamorphic rocks
-
metamorphic rocks
-
metasedimentary rocks
-
metapelite (1)
-
metasandstone (1)
-
-
-
turbidite (12)
-
-
minerals
-
silicates
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
-
-
Primary terms
-
absolute age (3)
-
Africa
-
East Africa
-
Tanzania (1)
-
-
North Africa
-
Morocco (1)
-
-
-
Arctic Ocean (1)
-
Arctic region
-
Greenland
-
West Greenland (1)
-
-
-
Asia
-
Far East
-
Indonesia
-
Sunda Arc (1)
-
-
Japan
-
Honshu
-
Chiba Peninsula (2)
-
-
-
-
-
Atlantic Ocean
-
East Atlantic (1)
-
North Atlantic
-
Faeroe-Shetland Basin (1)
-
Gulf of Cadiz (2)
-
Gulf of Mexico (2)
-
Little Bahama Bank (1)
-
Northeast Atlantic (2)
-
Northwest Atlantic
-
Demerara Rise (1)
-
-
Rockall Plateau (1)
-
Rockall Trough (1)
-
-
South Atlantic
-
Southwest Atlantic (2)
-
-
-
Australasia
-
New Zealand (1)
-
-
Canada
-
Eastern Canada
-
Newfoundland and Labrador
-
Newfoundland
-
Avalon Peninsula (1)
-
-
-
-
Mackenzie Mountains (1)
-
Western Canada
-
Northwest Territories (1)
-
-
-
carbon
-
C-14 (2)
-
-
Caribbean region
-
West Indies
-
Bahamas (1)
-
-
-
Cenozoic
-
Quaternary
-
Holocene
-
upper Holocene (1)
-
-
Kazusa Group (1)
-
Pleistocene
-
upper Pleistocene
-
Weichselian
-
upper Weichselian
-
Younger Dryas (1)
-
-
-
-
-
-
Tertiary
-
Neogene
-
Miocene (2)
-
Pliocene
-
upper Pliocene (1)
-
-
-
Paleogene
-
Eocene (1)
-
Paleocene (1)
-
-
-
-
clay mineralogy (1)
-
climate change (2)
-
continental drift (1)
-
continental slope (1)
-
data processing (1)
-
Europe
-
Southern Europe
-
Iberian Peninsula
-
Portugal (1)
-
-
Italy
-
Apennines (1)
-
Emilia-Romagna Italy
-
Parma Italy (1)
-
-
Marches Italy
-
Pesaro Italy (1)
-
-
Tuscany Italy
-
Pisa Italy (1)
-
Siena Italy (1)
-
-
-
-
Western Europe
-
Scandinavia
-
Denmark (1)
-
-
United Kingdom
-
Great Britain
-
Scotland (1)
-
Wales
-
Welsh Basin (1)
-
-
-
-
-
-
faults (3)
-
geochemistry (1)
-
geomorphology (1)
-
geophysical methods (16)
-
glacial geology (1)
-
hydrology (1)
-
ichnofossils (1)
-
igneous rocks
-
volcanic rocks (1)
-
-
Indian Ocean
-
Mid-Indian Ridge
-
Southeast Indian Ridge (1)
-
-
-
Invertebrata
-
Protista
-
Foraminifera
-
Rotaliina
-
Globigerinacea
-
Globigerinidae
-
Globigerinoides (1)
-
-
-
-
-
-
-
isotopes
-
radioactive isotopes
-
C-14 (2)
-
-
stable isotopes
-
O-18/O-16 (2)
-
-
-
marine geology (1)
-
Mediterranean region (1)
-
Mediterranean Sea
-
West Mediterranean (3)
-
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (2)
-
-
Triassic (2)
-
-
metamorphic rocks
-
metasedimentary rocks
-
metapelite (1)
-
metasandstone (1)
-
-
-
Mexico
-
Baja California (1)
-
-
North America
-
Great Lakes
-
Lake Superior (1)
-
-
-
ocean circulation (5)
-
Ocean Drilling Program
-
Leg 105
-
ODP Site 645 (1)
-
-
Leg 181
-
ODP Site 1122 (1)
-
-
-
ocean floors (8)
-
oceanography (4)
-
oil and gas fields (1)
-
orogeny (1)
-
oxygen
-
O-18/O-16 (2)
-
-
Pacific Ocean
-
East Pacific
-
Southeast Pacific (1)
-
-
South Pacific
-
Southeast Pacific (1)
-
-
West Pacific
-
Indonesian Seas (1)
-
-
-
paleoclimatology (6)
-
paleoecology (1)
-
paleogeography (2)
-
paleomagnetism (1)
-
Paleozoic
-
Silurian
-
Lower Silurian
-
Llandovery
-
Aberystwyth Grits (1)
-
-
-
-
-
palynomorphs
-
Dinoflagellata (1)
-
-
petroleum (2)
-
plate tectonics (2)
-
Precambrian
-
upper Precambrian
-
Proterozoic
-
Neoproterozoic
-
Ediacaran (3)
-
Vendian (2)
-
-
Windermere System (1)
-
-
-
-
problematic fossils (1)
-
sea-level changes (1)
-
sedimentary petrology (1)
-
sedimentary rocks
-
carbonate rocks
-
chalk (1)
-
limestone (1)
-
-
chemically precipitated rocks
-
evaporites
-
salt (1)
-
-
-
clastic rocks
-
conglomerate (2)
-
marl (1)
-
mudstone (3)
-
sandstone (3)
-
shale (1)
-
-
-
sedimentary structures
-
bedding plane irregularities
-
ripple marks (2)
-
-
biogenic structures
-
bioturbation (2)
-
lebensspuren (1)
-
-
graded bedding (1)
-
planar bedding structures
-
bedding (1)
-
cross-bedding (1)
-
laminations (4)
-
ripple drift-cross laminations (1)
-
-
primary structures (1)
-
seismites (1)
-
soft sediment deformation
-
olistostromes (1)
-
-
turbidity current structures (1)
-
-
sedimentation (10)
-
sediments
-
clastic sediments
-
clay (3)
-
drift (4)
-
gravel (2)
-
mud (3)
-
sand (4)
-
silt (4)
-
-
marine sediments (11)
-
-
slope stability (1)
-
South America
-
Argentina (1)
-
French Guiana (1)
-
Surinam (1)
-
Uruguay (1)
-
-
Southern Ocean (2)
-
stratigraphy (2)
-
tectonophysics (1)
-
United States
-
Michigan
-
Michigan Upper Peninsula
-
Keweenaw Peninsula (1)
-
-
-
Mississippi River (1)
-
-
-
sedimentary rocks
-
contourite (32)
-
flysch (1)
-
sedimentary rocks
-
carbonate rocks
-
chalk (1)
-
limestone (1)
-
-
chemically precipitated rocks
-
evaporites
-
salt (1)
-
-
-
clastic rocks
-
conglomerate (2)
-
marl (1)
-
mudstone (3)
-
sandstone (3)
-
shale (1)
-
-
-
siliciclastics (2)
-
tempestite (1)
-
turbidite (12)
-
volcaniclastics (1)
-
-
sedimentary structures
-
channels (1)
-
sedimentary structures
-
bedding plane irregularities
-
ripple marks (2)
-
-
biogenic structures
-
bioturbation (2)
-
lebensspuren (1)
-
-
graded bedding (1)
-
planar bedding structures
-
bedding (1)
-
cross-bedding (1)
-
laminations (4)
-
ripple drift-cross laminations (1)
-
-
primary structures (1)
-
seismites (1)
-
soft sediment deformation
-
olistostromes (1)
-
-
turbidity current structures (1)
-
-
-
sediments
-
contourite (32)
-
sediments
-
clastic sediments
-
clay (3)
-
drift (4)
-
gravel (2)
-
mud (3)
-
sand (4)
-
silt (4)
-
-
marine sediments (11)
-
-
siliciclastics (2)
-
tempestite (1)
-
turbidite (12)
-
volcaniclastics (1)
-
-
soils
-
paleosols (1)
-
Hybrid turbidite–contourite systems of the Tanzanian margin
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
M. Nemčok, L. Loncke, S. Rybár, A. Maillard, S. T. Sinha, C. Basile, S. A. Hermeston, W. R. Roest, L. Ledvényiová, G. Bayon, V. Gaullier, F. Pattier, M. Mercier de Lépinay, C. Grall, L. Droz, T. Marsset, P. Giresse, J. C. Caprais, C. Cathalot, D. Graindorge, A. Heuret, J. F. Lebrun, S. Bermell, B. Marcaillou, C. Sotin, B. Hebert, M. Patriat, M. A. Bassetti, C. Tallobre, R. Buscail, X. Durrieu de Madron, F. BourrinThe 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. AbstractThe 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.
A contourite drift system on the Baffin Bay–West Greenland margin linking Pliocene Arctic warming to poleward ocean circulation
Volcanosedimentary paleoenvironments of Ediacaran fossils in Newfoundland
Contourite processes associated with the Mediterranean Outflow Water after its exit from the Strait of Gibraltar: Global and conceptual implications
PALEOENVIRONMENTAL AND PALEOCLIMATIC IMPLICATIONS OF ENHANCED HOLOCENE DISCHARGE FROM THE MISSISSIPPI RIVER BASED ON THE SEDIMENTOLOGY AND GEOCHEMISTRY OF A DEEP CORE (JPC-26) FROM THE GULF OF MEXICO
Seismic geomorphology of early North Atlantic sediment waves, offshore northwest Africa
Magnetic-Fabric Analysis As A Tool To Constrain Mechanisms of Deep-Water Mudstone Deposition In the Marnoso Arenacea Formation (Miocene, Italy)
Facies and ichnology of an Upper Cretaceous chalk contourite drift complex, eastern Denmark, and the validity of contourite facies models
Onset of North Atlantic Deep Water production coincident with inception of the Cenozoic global cooling trend
Contourite depositional system on the Argentine Slope: An exceptional record of the influence of Antarctic water masses
Paleoenvironmental and basin analysis of the late Neoproterozoic (Ediacaran) upper Conception and St. John’s groups, west Conception Bay, Newfoundland
The petrology and provenance of sand in the Bounty submarine fan, New Zealand
José Arribas, Shawn A. Shapiro, Mark J. Johnsson, Kathleen M. Marsaglia, Salvatore Critelli, Lionel CarterOff the east coast of South Island, New Zealand, the Bounty Fan lies in the most seaward axial deep of the Bounty Trough, a remnant continental rift. The north levee of the Bounty Channel was cored at Ocean Drilling Program (ODP) Site 1122 on Leg 181. The 617 m section, which is divided into three units and nine subunits, consists of a Quaternary fan turbidite sequence that transitions downward into a Pleistocene to Pliocene mixed turbidite to contourite facies, which unconformably overlies a Miocene contourite-pelagic succession. Petrographic analysis (point counts) of 55 fine to very fine sand samples across the cored interval shows them to be quartzofeldspathic with moderate mica and minor metamorphic lithic components (mean values = Q44F44L12, Qm50K3P47, Lm70Lv4Ls26, total%mica14). Mean recalculated parameters for Site 1122 units and subunits cluster on QFL, QmKP, and LmLvLs ternary plots with little compositional variation. Proportions of biotite, muscovite, chlorite, and various metamorphic lithic types also show little compositional variation among the units and subunits of Site 1122. Furthermore, there are no significant trends among thickness, grain size, composition, and depth of Site 1122 sand samples, except that thicker beds tend to contain slightly more metamorphic rock fragments. The generally homogeneous composition of Site 1122 sand indicates that it may have had a relatively uniform source back into the early Miocene. Thus, the up-section change from sandy contourite to turbidite deposits at Site 1122 is not reflected in sand composition. This suggests that the sand provenance remained constant while the depositional processes of sand at Site 1122 changed. Sand detrital modes at Site 1122 most closely match those of the Clutha River, especially in terms of QFL, QmKP, mica, and lithic proportions, suggesting that it was a major source of sand at Site 1122. However, admixing of sand from the Waitaki River and other sources cannot be completely ruled out.