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NARROW
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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Angola (4)
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Morocco
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Southern Africa
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West Africa
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Atlantic Ocean
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Southern Europe
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Iberian Peninsula
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Spain
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Ionian Zone (1)
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Italy
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Western Europe
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France
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Ireland
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Scandinavia
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Norway
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United Kingdom
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Great Britain
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England
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Wales
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Fraser River (1)
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Indian Ocean
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Indian Ocean Islands
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International Ocean Discovery Program
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Expedition 354 (1)
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Median Tectonic Line (1)
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Mediterranean Sea
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East Mediterranean
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Mediterranean Ridge (1)
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Mexico
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Yucatan Mexico (1)
-
-
NanTroSEIZE
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IODP Site C0011 (1)
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IODP Site C0012 (1)
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-
North America
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Appalachian Basin (1)
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Appalachians
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Northern Appalachians (3)
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Basin and Range Province (1)
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Canadian Shield
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Protista
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Foraminifera
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Rotaliina
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Buliminacea
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Uvigerinidae
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Uvigerina (1)
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Cassidulinacea
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Anomalinidae
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Cibicidoides
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Cibicidoides wuellerstorfi (1)
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Globigerinacea
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Globigerinidae
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Globigerinoides
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Globigerinoides ruber (1)
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Neogloboquadrina
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Neogloboquadrina dutertrei (1)
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Orbitoidacea
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Amphistegina (1)
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Radiolaria (2)
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Metazoa (1)
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microfossils (29)
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palynomorphs
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Dinoflagellata (5)
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miospores
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pollen (2)
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Plantae
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algae
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Chlorophyta
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Chlorophyceae
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Dasycladaceae (1)
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Coccolithophoraceae (1)
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nannofossils (3)
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thallophytes (3)
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geochronology methods
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Ar/Ar (2)
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optically stimulated luminescence (1)
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paleomagnetism (2)
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tephrochronology (1)
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U/Pb (8)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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lower Holocene (2)
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upper Holocene (1)
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Kazusa Group (1)
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Pleistocene
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lower Pleistocene (2)
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upper Pleistocene
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Barents ice sheet (1)
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Wurm (1)
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upper Quaternary
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Scandinavian ice sheet (1)
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Tertiary
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lower Tertiary (1)
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Maikop Series (2)
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Neogene
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Capistrano Formation (2)
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Miocene
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Antelope Shale (2)
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lower Miocene (2)
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middle Miocene
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Langhian (1)
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Serravallian (2)
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Stevens Sandstone (1)
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upper Miocene
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Messinian (2)
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Tortonian (3)
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Pliocene
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lower Pliocene (1)
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upper Pliocene (1)
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Paleogene
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Barail Group (1)
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Eocene
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Annot Sandstone (1)
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lower Eocene
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Ypresian (1)
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Matilija Formation (2)
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middle Eocene
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Lutetian (1)
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Tyee Formation (3)
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lower Paleogene (3)
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Oligocene
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Frio Formation (1)
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Hackberry Formation (1)
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Paleocene
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middle Paleocene (1)
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upper Paleocene (3)
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Refugian (1)
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Wilcox Group (2)
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Shahejie Formation (1)
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upper Tertiary (2)
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upper Cenozoic (1)
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Laurentide ice sheet (1)
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Mesozoic
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Cretaceous
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Chatsworth Formation (1)
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Lower Cretaceous
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Albian (6)
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Aptian (2)
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Barremian (1)
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Berriasian (3)
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Hauterivian (2)
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Torok Formation (1)
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Valanginian (1)
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Upper Cretaceous
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Campanian (5)
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Cenomanian (1)
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Coniacian (1)
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Dawson Canyon Formation (1)
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Fox Hills Formation (2)
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Izumi Group (1)
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Kodiak Formation (1)
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Lance Formation (2)
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Lewis Shale (3)
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Maestrichtian (7)
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Rosario Formation (2)
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Senonian (5)
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Turonian (1)
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Wyandot Formation (1)
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Franciscan Complex (5)
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Great Valley Sequence (4)
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Jurassic
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Heather Formation (1)
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Lower Jurassic
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Toarcian (1)
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upper Liassic (1)
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Middle Jurassic
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Aalenian (1)
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Upper Jurassic
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Kimmeridge Clay (4)
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Kimmeridgian (2)
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Naknek Formation (1)
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Oxfordian (1)
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Portlandian (2)
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Tithonian (1)
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Volgian (1)
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lower Mesozoic (1)
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Triassic
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upper Mesozoic (3)
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Paleozoic
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Cambrian
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Lower Cambrian (3)
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Upper Cambrian (1)
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Carboniferous
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Jackfork Group (5)
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Lower Carboniferous
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Dinantian (2)
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Mississippian
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Stanley Group (1)
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Upper Mississippian
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Serpukhovian (1)
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Namurian (4)
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Pennsylvanian
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Lower Pennsylvanian
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Bashkirian (1)
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Marble Falls Group (1)
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Middle Pennsylvanian
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Atokan
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Atoka Formation (3)
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Morrow Formation (1)
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Red Fork Sandstone (2)
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Strawn Series (2)
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Upper Pennsylvanian
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Canyon Group (1)
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Missourian (4)
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Virgilian (3)
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Springer Formation (1)
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Upper Carboniferous (4)
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Devonian
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Middle Devonian (1)
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Upper Devonian
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Brallier Shale (1)
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Chemung Formation (1)
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Laborcita Formation (2)
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Ordovician
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Lower Ordovician
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Arenigian (1)
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Martinsburg Formation (1)
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Middle Ordovician
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Cloridorme Formation (1)
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Upper Ordovician (1)
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Permian
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Guadalupian
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Bell Canyon Formation (1)
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Brushy Canyon Formation (1)
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Cherry Canyon Formation (1)
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Delaware Mountain Group (1)
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Lower Permian
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Abo Formation (2)
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Cherry Canyon Formation (1)
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Wolfcampian (2)
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Rotliegendes (1)
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Upper Permian
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Zechstein (1)
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Silurian (1)
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Phanerozoic (1)
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Precambrian
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Archean
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Fig Tree Group (1)
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Paleoarchean (1)
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Warrawoona Group (1)
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Johnnie Formation (1)
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middle Precambrian (1)
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upper Precambrian
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Proterozoic
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Huronian
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Gowganda Formation (1)
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Miette Group (1)
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Neoproterozoic
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Ediacaran
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Wonoka Formation (1)
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Hadrynian (2)
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Horsethief Creek Group (1)
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Vendian (1)
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Wilpena Group (1)
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Paleoproterozoic (1)
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Yellowjacket Formation (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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ultramafics (1)
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volcanic rocks
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andesites (1)
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basalts
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pyroclastics
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tuff (2)
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ophiolite (4)
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metamorphic rocks
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metamorphic rocks
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gneisses (2)
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ophiolite (4)
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turbidite (150)
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minerals
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carbonates
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hydrates (1)
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oxides
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silicates
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framework silicates
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feldspar group
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alkali feldspar
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K-feldspar (1)
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silica minerals
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quartz (2)
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zeolite group
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clinoptilolite (1)
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heulandite (1)
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orthosilicates
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nesosilicates
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olivine group
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olivine (1)
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zircon group
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zircon (8)
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sorosilicates
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pumpellyite group
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pumpellyite (1)
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sheet silicates
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chlorite group (1)
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clay minerals
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kaolinite (1)
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smectite (2)
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mica group
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glauconite (2)
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muscovite (1)
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sulfates
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gypsum (1)
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sulfides
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pyrite (1)
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Primary terms
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absolute age (19)
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Africa
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Southern Africa
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Transvaal region (1)
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West Africa
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Arctic region
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Asia
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Far East
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Indonesia
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Japan
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Atlantic Ocean
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South Atlantic
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Atlantic region (1)
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Australasia
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Australia
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biogeography (1)
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Canada
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carbon
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organic carbon (2)
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Caribbean region
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Cenozoic
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Quaternary
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Holocene
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Kazusa Group (1)
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Pleistocene
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upper Pleistocene
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upper Quaternary
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Scandinavian ice sheet (1)
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Tertiary
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lower Tertiary (1)
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Maikop Series (2)
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Neogene
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Capistrano Formation (2)
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Miocene
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Antelope Shale (2)
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lower Miocene (2)
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middle Miocene
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Langhian (1)
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Serravallian (2)
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Stevens Sandstone (1)
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upper Miocene
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Messinian (2)
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Tortonian (3)
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Pliocene
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lower Pliocene (1)
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upper Pliocene (1)
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Paleogene
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Barail Group (1)
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Eocene
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Annot Sandstone (1)
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lower Eocene
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Ypresian (1)
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Matilija Formation (2)
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middle Eocene
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Lutetian (1)
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Tyee Formation (3)
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lower Paleogene (3)
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Oligocene
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Frio Formation (1)
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Hackberry Formation (1)
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Paleocene
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middle Paleocene (1)
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upper Paleocene (3)
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Refugian (1)
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Wilcox Group (2)
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Shahejie Formation (1)
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upper Tertiary (2)
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Deep Sea Drilling Project
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IPOD
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DSDP Site 603 (1)
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Leg 54 (1)
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Leg 63
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DSDP Site 471 (1)
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Leg 77
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DSDP Site 537 (1)
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Leg 93 (1)
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Leg 95 (1)
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Leg 96
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DSDP Site 615 (1)
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Leg 10
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DSDP Site 96 (1)
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Leg 18
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DSDP Site 178 (1)
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Leg 22
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DSDP Site 211 (1)
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DSDP Site 216 (1)
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DSDP Site 217 (1)
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DSDP Site 218 (1)
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Leg 23
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DSDP Site 224 (1)
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Leg 42B
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DSDP Site 379 (2)
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DSDP Site 381 (1)
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deformation (11)
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faults (48)
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submarine fans
Simple model, complex strata: 2-D numerical forward model analysis of heterogeneity and controls in submarine fan systems Available to Purchase
How many turbidity currents pass through a submarine channel during its lifespan? Available to Purchase
Deep-water fan hierarchy: assumptions, evidence, and numerical modeling analysis Available to Purchase
Exploring the predictive power of seismic geomorphology to assess sedimentary characteristics of gravity-flow deposits: examples from offshore East and West Africa reservoirs Available to Purchase
Abstract This research seeks to test the hypothesis that the rheology of submarine gravity-flows influences the planform geometry of associated fan lobe deposits. If this control exists, seismic geomorphology has the potential to predict the sedimentary characteristics of these deposits by analysing relatively simple seismic outputs such as time structure maps and amplitude maps. This predictive power could potentially aid the identification of prospective reservoirs through automated processes of seismic interpretation. In this work, Upper Cretaceous and Neogene deep-water reservoirs from East and West Africa with porosity in excess of 20% and multi-Darcy permeability were analysed. The overall external geometry of the reservoirs was described by integrating seismic amplitude extractions, structure and isochron maps derived from high-quality 3D seismic data. The maps were generated from detailed interpretation of the top and base reservoir reflections. Core photos of the reservoirs were integrated into the seismic project and their examination allowed the identification of dominant sedimentary facies, enabling a proposal for the classification of these deposits in terms of flow processes. The research indicates that the confinement of flows exerts an obvious control on the shape of the deposits and results in sedimentary bodies with marked elongation at the seismic scale. However, analysis of the reservoirs at the core scale indicated that they are dominated by massive, poorly sorted, medium- to coarse-grained sandstones, commonly with floating oversize clasts, as well as beds with disrupted laminae and sandy conglomerates. These characteristics may indicate ‘depositional freezing’ from high-density flows with yield strength, which may also have contributed to the limited lateral spread of the deposits analysed. The research also highlights the importance of the non-unique relationship between sedimentary processes and external geometries of the resulting deposits at the seismic scale. This means that deposits with similar geometries may have markedly different sedimentary characteristics. This work highlights the increasing importance of integrating detailed seismic geomorphology studies with an accurate examination of core data to validate models of gravity flow processes and test their predictive value.
Micropaleontological Evidence of A Submarine Fan in the Lower Coaledo Formation, Southwestern Oregon, USA Open Access
Flow transformations, Mud Partitioning, and the Variable Stratigraphic Architecture of Basin-Floor Fan Fringes Available to Purchase
Multi-phase ecological change on Indian subcontinent from the late Miocene to Pleistocene recorded in the Nicobar Fan Open Access
Stratigraphic architecture and distribution patterns of submarine fan-reservoir elements: insights derived from the Pliocene and Pleistocene Bengal Fan Available to Purchase
Multiple scours and upward fining caused by hydraulic jumps: implications for the recognition of cyclic steps in the deepwater stratigraphic record Available to Purchase
Petrology of Bengal Fan turbidites (IODP Expeditions 353 and 354): provenance versus diagenetic control Available to Purchase
Controls on grain-size variability in the Holocene fill of the Indus Submarine Canyon Available to Purchase
The Sediment Budget Estimator (SBE): A process model for the stochastic estimation of fluxes and budgets of sediment through submarine channel systems Available to Purchase
The Zambezi deep-sea fan: mineralogical, REE, Zr/Hf, Nd-isotope, and zircon-age variability in feldspar-rich passive-margin turbidites Available to Purchase
Multiple trend integration method based on depositional model and its application in glutenite reservoir modeling Available to Purchase
How did the world’s largest submarine fan in the Bay of Bengal grow and evolve at the subfan scale? Available to Purchase
Early Cretaceous to Paleogene sandstone provenance and sediment-dispersal systems of the Cuicateco terrane, Mexico Available to Purchase
ABSTRACT Sandstone petrography, detrital zircon geochronology, and sedimentology of Lower Cretaceous to Paleocene strata in the Cuicateco terrane of southern Mexico indicate an evolution from extensional basin formation to foreland basin development. The Early Cretaceous extensional basin is characterized by deposition of deep-marine fans and channels, which were mainly sourced from Mesoproterozoic and Permian crystalline rocks of the western shoulder of the rift basin. Some submarine fans, especially in the northern Cuicateco terrane, record an additional source in the Early Cretaceous (ca. 130 Ma) continental arc. The fans were fed by fluvial systems in updip parts of the extensional basin system. The transition from middle Cretaceous tectonic quiescence to Late Cretaceous shortening is recorded by the Turonian–Coniacian Tecamalucan Formation. The Tecamalucan Formation is interpreted as pre-orogenic deposits that represent submarine-fan deposits sourced from Aptian–Albian carbonate platform and pre-Mesozoic basement. The foreland basin in the Cuicateco terrane was established by the Maastrichtian, when foredeep strata of the Méndez Formation were deposited in the Cuicateco terrane, Veracruz basin, and across the western Gulf of Mexico, from Tampico to Tabasco. In the Zongolica region, these strata were derived from a contemporaneous volcanic arc (100–65 Ma) located to the west of the basin, the accreted Guerrero terrane (145–120 Ma), and the fold belt itself. By the Paleocene, sediments were transported to the foreland basin by drainages sourced in southwestern Mexico, such as the Late Cretaceous magmatic rocks of the Sierra Madre del Sur, and the Chortis block.