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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Central Africa
-
Angola (1)
-
-
North Africa
-
Egypt
-
Nile Delta (2)
-
-
Libya
-
Sirte Basin (1)
-
-
-
Southern Africa
-
Karoo Basin (1)
-
South Africa
-
Cape fold belt (1)
-
KwaZulu-Natal South Africa
-
Zululand (1)
-
-
-
-
West Africa
-
Nigeria
-
Niger Delta (9)
-
-
-
-
Antarctica
-
Ellsworth Land
-
Ellsworth Mountains (1)
-
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Transantarctic Mountains (1)
-
West Antarctica (1)
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Arctic Ocean
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Barents Sea (2)
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Norwegian Sea
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Voring Plateau (1)
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Arctic region
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Greenland
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East Greenland (1)
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Russian Arctic
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Novaya Zemlya (1)
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Svalbard
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Spitsbergen (2)
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Asia
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Arabian Peninsula
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Oman (1)
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Far East
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Borneo
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Brunei (6)
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East Malaysia
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Sarawak Malaysia (1)
-
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Kalimantan Indonesia
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Mahakam Delta (1)
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China
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Bohaiwan Basin (2)
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Hebei China (1)
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Indonesia
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Kalimantan Indonesia
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Mahakam Delta (1)
-
-
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Malaysia
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East Malaysia
-
Sarawak Malaysia (1)
-
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-
-
-
Atlantic Ocean
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North Atlantic
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Amazon Fan (1)
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Foz do Amazonas Basin (1)
-
Georges Bank basin (1)
-
Gulf of Guinea (2)
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Gulf of Mexico
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De Soto Canyon (1)
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Eugene Island Block 330 Field (1)
-
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North Sea
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Viking Graben (1)
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Northwest Atlantic (1)
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South Atlantic
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Santos Basin (1)
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Australasia
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Australia
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Queensland Australia (2)
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South Australia
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Fleurieu Peninsula (1)
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Kangaroo Island (1)
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Kanmantoo Trough (1)
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Tasmania Australia (1)
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Western Australia
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Pilbara (1)
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Tasman orogenic zone (1)
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Bowen Basin (1)
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Campos Basin (1)
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Canada
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Eastern Canada
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Maritime Provinces
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Ontario
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Sudbury Structure (1)
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Quebec (1)
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Western Canada
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Alberta
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British Columbia (1)
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Northwest Territories
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Mackenzie Delta (1)
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Caribbean region
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West Indies
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Antilles
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Greater Antilles
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Jamaica (2)
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Bahamas (1)
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Central Graben (1)
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Colorado River (1)
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Commonwealth of Independent States
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Russian Federation
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Arkhangelsk Russian Federation
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Novaya Zemlya (1)
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Russian Arctic
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Novaya Zemlya (1)
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Timan-Pechora region (1)
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Urals
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Corpus Christi Bay (3)
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Europe
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Alps
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Western Alps
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Vercors (1)
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Arkhangelsk Russian Federation
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Novaya Zemlya (1)
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Pyrenees
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Spain
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Italy (1)
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Timan-Pechora region (1)
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Western Europe
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France
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Alpes-Maritimes France (1)
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Vercors (1)
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Isere France (1)
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Ireland
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Clare Ireland (1)
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Scandinavia
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Norway (4)
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United Kingdom
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Great Britain
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England (3)
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Grand Canyon (1)
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High Island (1)
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Huanghua Depression (1)
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Indian Ocean
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Great Australian Bight (1)
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Mid-Indian Ridge (1)
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West Indian Ocean (1)
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Kutei Basin (1)
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Lake District (1)
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Lake Mead (1)
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Macuspana Basin (1)
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Malay Archipelago
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Borneo
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Brunei (6)
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East Malaysia
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Sarawak Malaysia (1)
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Kalimantan Indonesia
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Mahakam Delta (1)
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Mediterranean region
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Mediterranean Sea
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Mexico
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Mustang Island (1)
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North America
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Appalachians (2)
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Basin and Range Province
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Great Basin (1)
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Great Lakes
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Gulf Coastal Plain (31)
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Rio Grande Rift (2)
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North Slope (1)
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Pacific Coast (1)
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Pacific Ocean
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North Pacific
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Yellow Sea
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West Pacific
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Northwest Pacific
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South China Sea (1)
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Rio Grande (1)
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South America
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Brazil (2)
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Southern Ocean
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United States
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Alaska
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Ventura County California
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Iowa (1)
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Terrebonne Parish Louisiana (1)
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Vermilion Parish Louisiana (1)
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Michigan (1)
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Midcontinent (2)
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Minnesota (1)
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Mississippi Delta (2)
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Nevada
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Churchill County Nevada (1)
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New Jersey (1)
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New Mexico (2)
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New York
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New York Bight (1)
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North Dakota (1)
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Oklahoma (1)
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Oregon
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Klamath County Oregon (1)
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-
Pennsylvania (2)
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Southern U.S. (1)
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Southwestern U.S. (1)
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Texas
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DeWitt County Texas (1)
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Duval County Texas (1)
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Galveston County Texas
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Galveston Island (1)
-
-
Harris County Texas
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Houston Texas (1)
-
-
Hidalgo County Texas
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McAllen Ranch Field (1)
-
-
Houston County Texas (1)
-
Jackson County Texas (1)
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Live Oak County Texas (1)
-
Nueces County Texas (5)
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Reeves County Texas (1)
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San Marcos Arch (2)
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San Patricio County Texas (2)
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Starr County Texas (1)
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Zapata County Texas (3)
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commodities
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gold ores (1)
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lead ores (2)
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lead-zinc deposits (2)
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polymetallic ores (1)
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mineral deposits, genesis (2)
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oil and gas fields (21)
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petroleum
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natural gas (16)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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isotope ratios (3)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (3)
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metals
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oxygen
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O-18/O-16 (3)
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fossils
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Invertebrata
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Protista
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Foraminifera (4)
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-
microfossils (5)
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Plantae
-
algae
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nannofossils (1)
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thallophytes (1)
-
-
geochronology methods
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Ar/Ar (3)
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infrared stimulated luminescence (1)
-
optically stimulated luminescence (1)
-
paleomagnetism (2)
-
U/Pb (1)
-
-
geologic age
-
Cenozoic
-
Agbada Formation (2)
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene (2)
-
-
-
Saugus Formation (1)
-
Tertiary
-
Anahuac Formation (2)
-
middle Tertiary (1)
-
Neogene
-
Etchegoin Formation (1)
-
Miocene
-
lower Miocene (2)
-
middle Miocene (1)
-
upper Miocene
-
Messinian (2)
-
-
-
Pliocene
-
Cimmerian (1)
-
lower Pliocene (1)
-
-
-
Paleogene
-
Eocene
-
lower Eocene (7)
-
middle Eocene
-
Yegua Formation (1)
-
-
upper Eocene
-
Jackson Group (1)
-
-
-
Oligocene
-
Frio Formation (11)
-
middle Oligocene (6)
-
upper Oligocene (2)
-
Vicksburg Group (6)
-
-
Paleocene (2)
-
Wilcox Group (9)
-
-
-
-
Mesozoic
-
Cretaceous
-
Comanchean
-
Buda Limestone (1)
-
Glen Rose Formation (1)
-
-
Lower Cretaceous
-
Albian (2)
-
Aptian (1)
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Barremian (1)
-
Glen Rose Formation (1)
-
Missisauga Formation (1)
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Urgonian (1)
-
-
Macae Formation (1)
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Natih Formation (1)
-
Upper Cretaceous
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Buda Limestone (1)
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Campanian (3)
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Cenomanian (1)
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Coniacian (1)
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Maestrichtian (2)
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Santonian (1)
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Senonian (4)
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Turonian (1)
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Wahweap Formation (1)
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Jurassic
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Middle Jurassic (1)
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Upper Jurassic (5)
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Triassic
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Lower Triassic (1)
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Middle Triassic (1)
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Upper Triassic (1)
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-
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Paleozoic
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Cambrian
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Kanmantoo Group (1)
-
Upper Cambrian
-
Potsdam Sandstone (1)
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-
-
Carboniferous
-
Mississippian
-
Charles Formation (1)
-
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Namurian (1)
-
Pennsylvanian
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Middle Pennsylvanian
-
Atokan
-
Atoka Formation (1)
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-
-
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Upper Carboniferous (1)
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Devonian
-
Lower Devonian
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Oriskany Sandstone (1)
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-
Middle Devonian
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Onondaga Limestone (1)
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Tully Limestone (1)
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-
-
lower Paleozoic (2)
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Oquirrh Formation (1)
-
Ordovician
-
Lower Ordovician
-
Beekmantown Group (1)
-
-
Middle Ordovician (1)
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Trenton Group (1)
-
Upper Ordovician
-
Caradocian
-
Borrowdale Volcanic Group (1)
-
-
Red River Formation (1)
-
Trentonian (1)
-
-
-
Permian
-
Ecca Group (1)
-
Lower Permian (1)
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Rotliegendes (1)
-
Upper Permian
-
Zechstein (1)
-
-
-
Silurian (1)
-
upper Paleozoic (1)
-
-
Precambrian
-
Archean
-
Paleoarchean (1)
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Warrawoona Group (1)
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-
Chuar Group (1)
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Levack Gneiss (1)
-
Unkar Group (1)
-
upper Precambrian
-
Proterozoic
-
Mesoproterozoic (2)
-
Neoproterozoic (2)
-
Oronto Group (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
granites
-
I-type granites (1)
-
-
-
volcanic rocks
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andesites (1)
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basalts (1)
-
pyroclastics
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ash-flow tuff (1)
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ignimbrite (1)
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rhyolite tuff (1)
-
tuff (1)
-
-
rhyolites (3)
-
-
-
volcanic ash (2)
-
-
metamorphic rocks
-
metamorphic rocks
-
metaigneous rocks (1)
-
-
turbidite (6)
-
-
minerals
-
halides
-
chlorides
-
halite (1)
-
-
-
silicates
-
framework silicates
-
feldspar group (1)
-
silica minerals
-
quartz (2)
-
-
-
sheet silicates
-
clay minerals
-
kaolinite (1)
-
smectite (1)
-
-
illite (1)
-
-
-
sulfates
-
alunite (1)
-
anhydrite (1)
-
-
sulfides (1)
-
-
Primary terms
-
absolute age (3)
-
Africa
-
Central Africa
-
Angola (1)
-
-
North Africa
-
Egypt
-
Nile Delta (2)
-
-
Libya
-
Sirte Basin (1)
-
-
-
Southern Africa
-
Karoo Basin (1)
-
South Africa
-
Cape fold belt (1)
-
KwaZulu-Natal South Africa
-
Zululand (1)
-
-
-
-
West Africa
-
Nigeria
-
Niger Delta (9)
-
-
-
-
Antarctica
-
Ellsworth Land
-
Ellsworth Mountains (1)
-
-
Transantarctic Mountains (1)
-
West Antarctica (1)
-
-
Arctic Ocean
-
Barents Sea (2)
-
Norwegian Sea
-
Voring Plateau (1)
-
-
-
Arctic region
-
Greenland
-
East Greenland (1)
-
-
Russian Arctic
-
Novaya Zemlya (1)
-
-
Svalbard
-
Spitsbergen (2)
-
-
-
Asia
-
Arabian Peninsula
-
Oman (1)
-
-
Far East
-
Borneo
-
Brunei (6)
-
East Malaysia
-
Sarawak Malaysia (1)
-
-
Kalimantan Indonesia
-
Mahakam Delta (1)
-
-
-
China
-
Bohaiwan Basin (2)
-
Hebei China (1)
-
-
Indonesia
-
Kalimantan Indonesia
-
Mahakam Delta (1)
-
-
-
Malaysia
-
East Malaysia
-
Sarawak Malaysia (1)
-
-
-
-
-
Atlantic Ocean
-
North Atlantic
-
Amazon Fan (1)
-
Foz do Amazonas Basin (1)
-
Georges Bank basin (1)
-
Gulf of Guinea (2)
-
Gulf of Mexico
-
De Soto Canyon (1)
-
Eugene Island Block 330 Field (1)
-
-
North Sea
-
Viking Graben (1)
-
-
Northwest Atlantic (1)
-
-
South Atlantic
-
Santos Basin (1)
-
-
-
Australasia
-
Australia
-
Queensland Australia (2)
-
South Australia
-
Fleurieu Peninsula (1)
-
Kangaroo Island (1)
-
Kanmantoo Trough (1)
-
-
Tasmania Australia (1)
-
Western Australia
-
Pilbara (1)
-
-
-
Tasman orogenic zone (1)
-
-
barite deposits (1)
-
Canada
-
Eastern Canada
-
Maritime Provinces
-
Nova Scotia (2)
-
-
Ontario
-
Sudbury Structure (1)
-
-
Quebec (1)
-
-
Western Canada
-
Alberta
-
Peace River Arch (1)
-
-
British Columbia (1)
-
Canadian Cordillera (1)
-
Northwest Territories
-
Mackenzie Delta (1)
-
-
-
-
carbon
-
C-13/C-12 (1)
-
-
Caribbean region
-
West Indies
-
Antilles
-
Greater Antilles
-
Jamaica (2)
-
-
-
Bahamas (1)
-
-
-
Cenozoic
-
Agbada Formation (2)
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene (2)
-
-
-
Saugus Formation (1)
-
Tertiary
-
Anahuac Formation (2)
-
middle Tertiary (1)
-
Neogene
-
Etchegoin Formation (1)
-
Miocene
-
lower Miocene (2)
-
middle Miocene (1)
-
upper Miocene
-
Messinian (2)
-
-
-
Pliocene
-
Cimmerian (1)
-
lower Pliocene (1)
-
-
-
Paleogene
-
Eocene
-
lower Eocene (7)
-
middle Eocene
-
Yegua Formation (1)
-
-
upper Eocene
-
Jackson Group (1)
-
-
-
Oligocene
-
Frio Formation (11)
-
middle Oligocene (6)
-
upper Oligocene (2)
-
Vicksburg Group (6)
-
-
Paleocene (2)
-
Wilcox Group (9)
-
-
-
-
clay mineralogy (1)
-
climate change (1)
-
continental drift (1)
-
continental shelf (13)
-
continental slope (4)
-
crust (3)
-
data processing (4)
-
deformation (27)
-
diagenesis (4)
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earthquakes (2)
-
economic geology (19)
-
energy sources (11)
-
Europe
-
Alps
-
Western Alps
-
Dauphine Alps
-
Vercors (1)
-
-
-
-
Arkhangelsk Russian Federation
-
Novaya Zemlya (1)
-
-
Pyrenees
-
Spanish Pyrenees (2)
-
-
Southern Europe
-
Iberian Peninsula
-
Iberian pyrite belt (1)
-
Ossa-Morena Zone (1)
-
Portugal (1)
-
Spain
-
Aragon Spain (1)
-
Spanish Pyrenees (2)
-
-
-
Italy (1)
-
-
Timan-Pechora region (1)
-
Western Europe
-
France
-
Alpes-Maritimes France (1)
-
Ardeche France (1)
-
Dauphine Alps
-
Vercors (1)
-
-
Isere France (1)
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Vaucluse France (1)
-
-
Ireland
-
Clare Ireland (1)
-
-
Scandinavia
-
Norway (4)
-
-
United Kingdom
-
Great Britain
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England (3)
-
-
-
-
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faults (154)
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folds (31)
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fractures (3)
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geochemistry (3)
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geochronology (1)
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geomorphology (3)
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geophysical methods (52)
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geophysics (1)
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geosynclines (1)
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growth faults
Influence of multi-trend major fault reactivation during multiphase rifting: Beier Depression, Hailar Basin, NE China
Identification of sandstone-rich zones in upper bathyal, deep water environment on south Texas Gulf Coast
Mechanism Study of Hydrocarbon Differential Distribution Controlled by the Activity of Growing Faults in Faulted Basins: Case Study of Paleogene in the Wang Guantun Area, Bohai Bay Basin, China
Integrated geophysical analysis provides an alternate interpretation of the northern margin of the North American Midcontinent Rift System, Central Lake Superior
Quantitative diamondoid analysis indicates oil cosourcing from a deep petroleum system onshore Niger Delta Basin
Characterizing the growth of structures in three dimensions using patterns of deep-water fan and channel systems
The evolution of the Dowsing Graben System: implications for petroleum prospectivity in the UK Southern North Sea
Growth faults affecting depositional geometry, facies and sequence stratigraphy record on a carbonate platform edge (South Vercors Urgonian platform, SE France)
The Paleozoic Mount Carlton Deposit, Bowen Basin, Northeast Australia: Shallow High-Sulfidation Epithermal Au-Ag-Cu Mineralization Formed During Rifting
Archaean basin margin geology and crustal evolution: an East Pilbara traverse
Techniques to determine the kinematics of synsedimentary normal faults and implications for fault growth models
Abstract: Normal faults grow via a sympathetic increase in their displacement and length (‘isolated model’) or by rapid establishment of their near-final length prior to significant displacement accumulation (‘constant-length model’). The isolated model has dominated the structural geology literature for >30 years, although some 3D seismic data-based studies support the constant-length model. Because they make different predictions regarding rift development, and earthquake size and recurrence intervals in areas of continental extension, it is critical to test these models with data from natural examples. Here we outline a range of techniques that constrain the kinematics of synsedimentary normal faults and thus test competing fault growth models. We then apply these techniques to three seismically imaged faults, showing that, in general, they grew in accordance with the constant-length model, although periods of relatively minor tip propagation and coeval displacement accumulation, characteristics more consistent with the isolated model, also occurred. We argue that analysis of growth strata represents the best way to test competing fault growth models; most studies utilizing this approach support the constant-length fault model, suggesting it may be more widely applicable than is currently assumed. It is plausible that the very early development of large faults is, however, characterized by the development of faults that, pre-linkage, grow in accordance with the isolated model; we may simply lack the data resolution, especially in the subsurface, to resolve this very early stage of fault growth.
Feldspar dissolution, authigenic clays, and quartz cements in open and closed sandstone geochemical systems during diagenesis: Typical examples from two sags in Bohai Bay Basin, East China
The role of mechanical stratigraphy on normal fault growth across a Cretaceous carbonate multi-layer, central Texas (USA)
Recognizing pitfalls of seismic structure and amplitude anomalies in Osprey field, Brunei
Ubiquity of Wave-Dominated Deltas In Outer-Shelf Growth-Faulted Compartments
A constrained potential field data interpretation of the deep geometry of the Sudbury structure
Structural analysis of a salt-cored transfer zone in the South Timbalier Block 54, offshore Gulf of Mexico: Implications for restoration of salt-related extensional structures
Structural and stratigraphic feature delineation and facies distribution using seismic attributes and well log analysis applied to a Brazilian carbonate field
Abstract Nearly 2,000 feet of continuous core, combined with well log and 3-D seismic data, afford a rare opportunity to document variations of stratal architecture and related processes of shelf-edge, growth faulted deltaic systems through active and inactive periods of growth faults at the scale of 4 th -order sequences in the Frio Formation in Corpus Christi Bay. The growth fault history, examined by expansion ratio and T-Z plots, is divided into three different periods: (1) development (rapid subsidence, growth ratio > 2, steep and positive slope of T-Z plot); (2) less active to inactive (no growth, flat to negative slope of T-Z plot); and (3) maintenance (slow subsidence, growth ratio ~ 1, flat and positive slope of T-Z plot). These periods can be correlated to aggradational, repetitive fourth-order sequences of shoreface deposits, a transgressive unit composed of backstepping shoreface deposits, and several high-frequency progradational fourth-order sequences represented by wave-dominated, fluvial-influenced deltaic deposits. Varying subsidence rates serve as a dominant process in stratigraphic development of the Frio Formation, whereas sediment supply and eustatic sea-level changes are subordinate. The decameter-scale fourth-order sequences within the hanging wall section are grouped into two categories based on stratal architecture: (1) T-R cycles within development period of growth faults and (2) R cycles within maintenance period of growth faults. T-R cycles have complete transgressive and regressive intervals of similar thickness (R-T thickness ratio ~ 1.7), created by a balance between rapid sediment supply and rapid accommodation rate caused by high subsidence rate and low sea-level drop rate. This balance permits the possibility of preserving of both regressive and transgressive units and provides more time for modification of deltaic deposits by wave-storm processes. R cycles are dominated by regressive intervals containing minor transgressive intervals (R-T thickness ratio > 6). R cycles are the results of rapid progradation stacking as rapid sediment supply, slow subsidence and rapid sea-level drop. The reservoir quality of wave-dominated deposits is highly controlled by the percentage of the bioturbated beds that constitute permeability barriers. Within the period of development of growth faults, a high subsidence rate associated with high sediment rate may indicate a relative high energy environment with fewer bioturbated beds and better reservoir quality as documented by porosity and permeability data. Relatively more antithetic faults are present during the growth fault development period, making the interval structurally complex with potentially greater number of reservoir compartments.