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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Central Africa
-
Angola
-
Cabinda Angola (1)
-
-
-
North Africa
-
Atlas Mountains
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
Middle Atlas (1)
-
-
-
Egypt (2)
-
Morocco
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
Middle Atlas (1)
-
-
-
-
West Africa
-
Nigeria
-
Niger Delta (4)
-
-
-
-
Arctic Ocean
-
Barents Sea (1)
-
Beaufort Sea (3)
-
-
Arctic region
-
Svalbard (1)
-
-
Asia
-
Arabian Peninsula
-
Oman
-
Oman Mountains (1)
-
-
-
Far East
-
China
-
Bohaiwan Basin (1)
-
Shandong China
-
Jiyang Depression (1)
-
-
Xinjiang China (1)
-
-
-
Himalayas (1)
-
Indian Peninsula
-
India
-
Andhra Pradesh India (1)
-
Damodar Valley (1)
-
Godavari Valley (1)
-
Jharkhand India
-
Jharia coal field (1)
-
-
Mahanadi Valley (1)
-
Narmada Valley (1)
-
Pranhita-Godavari Valley (2)
-
-
-
Kyrgyzstan
-
Issyk-kul Lake (1)
-
-
Middle East
-
Cyprus
-
Troodos Massif (1)
-
-
Iran
-
Fars Iran (1)
-
-
Turkey
-
Anatolia (1)
-
North Anatolian Fault (1)
-
-
Zagros (2)
-
-
Tien Shan (2)
-
-
Atlantic Ocean
-
East Atlantic (2)
-
Equatorial Atlantic (1)
-
Mid-Atlantic Ridge
-
TAG hydrothermal field (1)
-
-
North Atlantic
-
Bay of Biscay (1)
-
Gulf of Mexico (9)
-
North Sea
-
Viking Graben (1)
-
-
Northeast Atlantic (1)
-
Northwest Atlantic
-
Hibernia Field (1)
-
-
Scotian Shelf (1)
-
TAG hydrothermal field (1)
-
-
South Atlantic
-
Espirito Santo Basin (1)
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Santos Basin (1)
-
-
-
Atlantic Ocean Islands
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Azores (1)
-
-
Atlantic region (1)
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Australasia
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Australia
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Lachlan fold belt (2)
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Queensland Australia (2)
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Victoria Australia
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Bendigo gold field (1)
-
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Western Australia
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Canning Basin (1)
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Carnarvon Basin (1)
-
-
-
New Zealand (1)
-
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Beaufort-Mackenzie Basin (1)
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Burgos Basin (1)
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Caledonides (1)
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Campos Basin (2)
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Canada
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Carswell Structure (1)
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Eastern Canada
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Maritime Provinces
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Nova Scotia
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Cape Breton Island (2)
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-
-
Newfoundland and Labrador
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Labrador (1)
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Newfoundland (3)
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Ontario (1)
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Quebec (1)
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Western Canada
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British Columbia (1)
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Canadian Cordillera (1)
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Northwest Territories
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Great Slave Lake (1)
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Mackenzie Delta (2)
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-
Saskatchewan (1)
-
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Cascade Range (1)
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Commonwealth of Independent States
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Kyrgyzstan
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Issyk-kul Lake (1)
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-
Russian Federation
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Timan-Pechora region (1)
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Death Valley (1)
-
Europe
-
Alps
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Western Alps
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Dauphine Alps
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Belledonne Massif (1)
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Pyrenees
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Spanish Pyrenees (2)
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Southern Europe
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Greece
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Greek Aegean Islands
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Hellenic Arc (1)
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Iberian Peninsula
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Spain
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Andalusia Spain
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Malaguide Complex (1)
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Aragon Spain
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Betic Cordillera (1)
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Iberian Mountains (1)
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Spanish Pyrenees (2)
-
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Italy
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Apennines
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Central Apennines (1)
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Northern Apennines (1)
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Calabria Italy (1)
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Marches Italy (1)
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Sardinia Italy (1)
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Umbria 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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Corsica (1)
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Dauphine Alps
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Belledonne Massif (1)
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Isere France (1)
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Ireland (1)
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Scandinavia
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Norway (5)
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United Kingdom
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Great Britain
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Scotland
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Great Glen Fault (1)
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Hebrides
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Inner Hebrides
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Raasay (1)
-
-
-
Highland region Scotland
-
Inverness-shire Scotland
-
Raasay (1)
-
-
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-
-
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Grand Banks (1)
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Henderson Mine (1)
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Huanghua Depression (1)
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Indian Ocean
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Exmouth Plateau (1)
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Red Sea
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Gulf of Suez (3)
-
-
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Krishna-Godavari Basin (1)
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Laguna Madre (1)
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Macuspana Basin (1)
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Malay Archipelago
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New Guinea (1)
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Maritimes Basin (2)
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Mediterranean region
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Aegean Islands
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Greek Aegean Islands
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Cyclades (1)
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Lesbos (1)
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-
-
Mediterranean Sea
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East Mediterranean
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Ionian Sea
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Gulf of Corinth (1)
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West Mediterranean
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Ligurian Sea (1)
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Mexico
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Campeche Mexico (1)
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Sierra Madre Oriental (1)
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Tabasco Mexico (1)
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Trans-Mexican volcanic belt (1)
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Mill Creek (1)
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North America
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Appalachians
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Piedmont (1)
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Basin and Range Province
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Great Basin (1)
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Canadian Shield
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Churchill Province
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Rae Province (1)
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Slave Province (2)
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Superior Province
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Abitibi Belt (1)
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-
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Great Lakes
-
Lake Erie (1)
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Lake Ontario (1)
-
-
Great Lakes region (1)
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Great Plains (1)
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Grenville Front (1)
-
Gulf Coastal Plain (6)
-
Kootenay Arc (1)
-
North American Cordillera
-
Canadian Cordillera (1)
-
-
Rio Grande Rift (7)
-
Rocky Mountains (3)
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Rocky Mountains foreland (1)
-
Transcontinental Arch (1)
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Western Overthrust Belt (1)
-
-
North Island (1)
-
North West Shelf (1)
-
Pacific Ocean
-
East Pacific
-
Northeast Pacific
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Juan de Fuca Ridge (1)
-
-
-
North Pacific
-
Northeast Pacific
-
Juan de Fuca Ridge (1)
-
-
Northwest Pacific
-
South China Sea
-
Gulf of Thailand (1)
-
-
Yellow Sea (1)
-
-
-
South Pacific
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Southwest Pacific
-
Hikurangi Trough (1)
-
-
-
West Pacific
-
Northwest Pacific
-
South China Sea
-
Gulf of Thailand (1)
-
-
Yellow Sea (1)
-
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Southwest Pacific
-
Hikurangi Trough (1)
-
-
-
-
Perth Basin (2)
-
Railroad Valley (1)
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Red Mountain (1)
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Richmond Basin (1)
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Ridge Basin (1)
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San Andreas Fault (1)
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San Luis Valley (1)
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Santa Maria Basin (1)
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South America
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Andes
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Southern Andes (1)
-
-
Brazil
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Sergipe-Alagoas Basin (1)
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Chile (2)
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Tierra del Fuego (1)
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Venezuela
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Eastern Venezuela (1)
-
-
-
United States
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Absaroka Fault (1)
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Albuquerque Basin (2)
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Allegheny Front (1)
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Amargosa Desert (1)
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Anadarko Basin (1)
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Arkoma Basin (1)
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Atlantic Coastal Plain (1)
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California
-
Inyo County California (1)
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Los Angeles County California (2)
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San Gabriel Fault (1)
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Santa Barbara Channel (1)
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Santa Barbara County California (1)
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Santa Monica Mountains (1)
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Southern California (2)
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Transverse Ranges (1)
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Ventura County California (1)
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Colorado
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Boulder County Colorado
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Boulder Colorado (1)
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Clear Creek County Colorado (1)
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Lake County Colorado
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Climax Colorado (1)
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Sedgwick County Colorado (1)
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Weld County Colorado
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Greeley Colorado (1)
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Colorado Plateau (1)
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Denver Basin (2)
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Eastern U.S. (1)
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Great Basin (1)
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Idaho
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Bonner County Idaho (1)
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Boundary County Idaho (2)
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Kansas
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Midcontinent (1)
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Montana (1)
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Nebraska (1)
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Elko County Nevada
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Pequop Mountains (1)
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Nevada Test Site (1)
-
Nye County Nevada (2)
-
-
New Mexico
-
Hidalgo County New Mexico (1)
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Socorro County New Mexico
-
Socorro New Mexico (1)
-
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Valencia County New Mexico (1)
-
-
Oklahoma
-
Custer County Oklahoma (1)
-
Dewey County Oklahoma (1)
-
Jackson County Oklahoma (1)
-
Kiowa County Oklahoma (1)
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Washita County Oklahoma (1)
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Wichita Mountains (1)
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South Dakota (1)
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Texas
-
Refugio County Texas (1)
-
-
Utah
-
Juab County Utah (1)
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Kane County Utah (1)
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Millard County Utah (1)
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Sevier Desert (1)
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Virginia
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Louisa County Virginia (1)
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Pittsylvania County Virginia (1)
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Washington
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Pend Oreille County Washington (2)
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Skamania County Washington
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Mount Saint Helens (1)
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West Virginia (1)
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Western U.S. (2)
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Wyoming (1)
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Yakima fold belt (1)
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Veracruz Basin (1)
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commodities
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energy sources (3)
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metal ores
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base metals (1)
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copper ores (3)
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gold ores (4)
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lead ores (1)
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lead-zinc deposits (1)
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manganese ores (1)
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molybdenum ores (1)
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uranium ores (2)
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zinc ores (1)
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mineral deposits, genesis (8)
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mineral exploration (1)
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oil and gas fields (9)
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petroleum
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natural gas (5)
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-
-
elements, isotopes
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carbon
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C-14 (1)
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organic carbon (2)
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hydrogen (1)
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isotope ratios (1)
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isotopes
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radioactive isotopes
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C-14 (1)
-
-
stable isotopes
-
O-18/O-16 (2)
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S-34/S-32 (3)
-
-
-
oxygen
-
O-18/O-16 (2)
-
-
sulfur
-
S-34/S-32 (3)
-
-
-
fossils
-
Chordata
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Vertebrata
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Tetrapoda
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Mammalia (1)
-
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-
-
Invertebrata
-
Protista
-
Foraminifera (3)
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-
-
microfossils (5)
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palynomorphs
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Dinoflagellata (1)
-
miospores
-
pollen (1)
-
-
-
Plantae
-
algae
-
nannofossils (2)
-
-
-
-
geochronology methods
-
Ar/Ar (3)
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fission-track dating (1)
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K/Ar (1)
-
paleomagnetism (4)
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Sr/Sr (1)
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tephrochronology (1)
-
-
geologic age
-
Cenozoic
-
Agbada Formation (1)
-
Quaternary
-
Holocene (2)
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Pleistocene
-
upper Pleistocene
-
Devensian (1)
-
-
-
-
Tertiary
-
Anahuac Formation (1)
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Climax Porphyry (1)
-
middle Tertiary (1)
-
Neogene
-
Miocene
-
Columbia River Basalt Group (1)
-
lower Miocene (2)
-
upper Miocene
-
Messinian (1)
-
-
-
Pliocene
-
lower Pliocene (1)
-
upper Pliocene (1)
-
-
-
Paleogene
-
Eocene (4)
-
Oligocene
-
Frio Formation (2)
-
middle Oligocene (2)
-
upper Oligocene (1)
-
Vicksburg Group (2)
-
-
Paleocene (2)
-
-
-
upper Cenozoic (2)
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Albian (3)
-
Aptian (2)
-
Barremian (1)
-
Hauterivian (1)
-
-
Macae Formation (1)
-
Upper Cretaceous
-
Campanian (1)
-
Cenomanian (2)
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Coniacian (1)
-
Niobrara Formation (2)
-
Pierre Shale (1)
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Santonian (3)
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Senonian (4)
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Turonian (1)
-
Wahweap Formation (1)
-
-
-
Jurassic
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Aztec Sandstone (1)
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Middle Jurassic (1)
-
Upper Jurassic
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Kimmeridgian (1)
-
-
-
Navajo Sandstone (2)
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Triassic
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Middle Triassic (1)
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-
-
Paleozoic
-
Cambrian (1)
-
Carboniferous
-
Mississippian
-
Boone Formation (1)
-
Macumber Formation (1)
-
Windsor Group (2)
-
-
Pennsylvanian
-
Cumberland Group (1)
-
-
Upper Carboniferous
-
Stephanian (1)
-
-
-
Devonian
-
Lower Devonian
-
Oriskany Sandstone (1)
-
-
Upper Devonian (1)
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Ordovician (1)
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Permian
-
Rotliegendes (1)
-
Upper Permian
-
Zechstein (1)
-
-
-
Silurian (1)
-
upper Paleozoic
-
Pictou Group (1)
-
-
-
Precambrian
-
Archean (3)
-
upper Precambrian
-
Proterozoic
-
Athabasca Formation (1)
-
Mesoproterozoic
-
Belt Supergroup (1)
-
-
Neoproterozoic (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
kimberlite (1)
-
plutonic rocks
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gabbros (1)
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granites (1)
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quartz monzonite (1)
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ultramafics (1)
-
-
volcanic rocks
-
pyroclastics
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ignimbrite (1)
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tuff (2)
-
-
-
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ophiolite (1)
-
-
metamorphic rocks
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metamorphic rocks
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cataclasites (1)
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eclogite (2)
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marbles (1)
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mylonites (3)
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phyllites (1)
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schists (1)
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ophiolite (1)
-
-
minerals
-
carbonates
-
calcite (1)
-
-
oxides
-
manganese oxides (1)
-
-
silicates
-
framework silicates
-
silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
chloritoid (1)
-
zircon group
-
zircon (1)
-
-
-
-
sheet silicates
-
chlorite group
-
chlorite (1)
-
sudoite (1)
-
-
clay minerals
-
dickite (1)
-
-
illite (1)
-
mica group
-
muscovite (1)
-
paragonite (1)
-
phengite (1)
-
-
pyrophyllite (1)
-
-
-
sulfates
-
gypsum (1)
-
-
-
Primary terms
-
absolute age (5)
-
Africa
-
Central Africa
-
Angola
-
Cabinda Angola (1)
-
-
-
North Africa
-
Atlas Mountains
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
Middle Atlas (1)
-
-
-
Egypt (2)
-
Morocco
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
Middle Atlas (1)
-
-
-
-
West Africa
-
Nigeria
-
Niger Delta (4)
-
-
-
-
Arctic Ocean
-
Barents Sea (1)
-
Beaufort Sea (3)
-
-
Arctic region
-
Svalbard (1)
-
-
Asia
-
Arabian Peninsula
-
Oman
-
Oman Mountains (1)
-
-
-
Far East
-
China
-
Bohaiwan Basin (1)
-
Shandong China
-
Jiyang Depression (1)
-
-
Xinjiang China (1)
-
-
-
Himalayas (1)
-
Indian Peninsula
-
India
-
Andhra Pradesh India (1)
-
Damodar Valley (1)
-
Godavari Valley (1)
-
Jharkhand India
-
Jharia coal field (1)
-
-
Mahanadi Valley (1)
-
Narmada Valley (1)
-
Pranhita-Godavari Valley (2)
-
-
-
Kyrgyzstan
-
Issyk-kul Lake (1)
-
-
Middle East
-
Cyprus
-
Troodos Massif (1)
-
-
Iran
-
Fars Iran (1)
-
-
Turkey
-
Anatolia (1)
-
North Anatolian Fault (1)
-
-
Zagros (2)
-
-
Tien Shan (2)
-
-
Atlantic Ocean
-
East Atlantic (2)
-
Equatorial Atlantic (1)
-
Mid-Atlantic Ridge
-
TAG hydrothermal field (1)
-
-
North Atlantic
-
Bay of Biscay (1)
-
Gulf of Mexico (9)
-
North Sea
-
Viking Graben (1)
-
-
Northeast Atlantic (1)
-
Northwest Atlantic
-
Hibernia Field (1)
-
-
Scotian Shelf (1)
-
TAG hydrothermal field (1)
-
-
South Atlantic
-
Espirito Santo Basin (1)
-
Santos Basin (1)
-
-
-
Atlantic Ocean Islands
-
Azores (1)
-
-
Atlantic region (1)
-
Australasia
-
Australia
-
Lachlan fold belt (2)
-
Queensland Australia (2)
-
Victoria Australia
-
Bendigo gold field (1)
-
-
Western Australia
-
Canning Basin (1)
-
Carnarvon Basin (1)
-
-
-
New Zealand (1)
-
-
Canada
-
Carswell Structure (1)
-
Eastern Canada
-
Maritime Provinces
-
Nova Scotia
-
Cape Breton Island (2)
-
-
-
Newfoundland and Labrador
-
Labrador (1)
-
Newfoundland (3)
-
-
Ontario (1)
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Quebec (1)
-
-
Western Canada
-
British Columbia (1)
-
Canadian Cordillera (1)
-
Northwest Territories
-
Great Slave Lake (1)
-
Mackenzie Delta (2)
-
-
Saskatchewan (1)
-
-
-
carbon
-
C-14 (1)
-
organic carbon (2)
-
-
Cenozoic
-
Agbada Formation (1)
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene
-
Devensian (1)
-
-
-
-
Tertiary
-
Anahuac Formation (1)
-
Climax Porphyry (1)
-
middle Tertiary (1)
-
Neogene
-
Miocene
-
Columbia River Basalt Group (1)
-
lower Miocene (2)
-
upper Miocene
-
Messinian (1)
-
-
-
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listric faults
Dynamic Modeling of the 2020 M w 6.0 Jiashi Earthquake: Constrained by Geodetic and Seismic Observations
Pliocene growth of the Dowlatabad syncline in Frontal Fars arc: Folding propagation across the Zagros Fold Belt, Iran
The enigma of the Albian Gap: spatial variability and the competition between salt expulsion and extension
Extensional fault–related folding of the North West shelf, Western Australia
Definition of the Churchill River Delta and its petroleum potential, offshore Labrador, Canada
The evolution of the Dowsing Graben System: implications for petroleum prospectivity in the UK Southern North Sea
Three-dimensional interpretation of tectono-sedimentary evolution and hydrocarbon prospectivity by the integration of airborne gravity gradiometer, regional gravity, magnetic, and two-dimensional seismic data in the Canning Basin, Western Australia
Practical and efficient three-dimensional structural restoration using an adaptation of the GeoChron model
Jequitinhonha Basin: Structural aspects, relationship with igneous activity, and hydrocarbon exudations
Kinematic Earthquake Ground‐Motion Simulations on Listric Normal Faults
Abstract: Rollover is the folding of the hanging-wall sedimentary record in response to slip on listric normal faults, and is a common feature of sediment-rich, gravity-driven tectonic provinces. Rollovers have been extensively studied by means of geometrical reconstruction, and numerical and analogue modelling. However, the detailed interaction between the kinematics of bounding listric normal faults and their hanging-wall deformation is not yet fully understood. In this study, we use 3D seismic-reflection data from the Forcados-Yokri area, western Niger Delta, Nigeria, to study the lateral linkage and landwards backstepping history of an array of listric normal faults, particularly focusing on their influence on the development and evolution of hanging-wall rollovers. Five individual, partly overlapping rollover structures have been studied with respect to their relative initiation and decay time, their spatial distribution, and their relationship to the tectonic history of their respective bounding faults. We demonstrate that the studied rollovers are highly dependent on the development of their bounding faults in terms of initiation time, lateral linkage, internal structural development and decay. Fault–rollover interaction is dynamic and changes through time depending on the temporal evolution of listric faults. Four genetic types of fault–rollover interaction were identified in this study: (1) the rotation of a rollover–crestal-collapse system, controlled by a changing lateral bounding-fault orientation during fault growth; (2) a stepwise shift of rollover–crestal-collapse systems associated with rollover abandonment, controlled by the initiation of a new fault in the footwall of an older structure; (3) a gradual shift of successive rollovers controlled by branching main faults; and (4) a general landwards and upwards migration of crestal-collapse faults within a rollover above stationary listric main faults.
Abstract: Salt is mechanically weaker than other sedimentary rocks in rift basins. It commonly acts as a strain localizer, and decouples supra- and sub-salt deformation. In the rift basins discussed in this paper, sub-salt faults commonly form wide and deep ramp synclines controlled by the thickness and strength of the overlying salt section, as well as by the shapes of the extensional faults, and the magnitudes and slip rates along the faults. Upon inversion of these rift basins, the inherited extensional architectures, and particularly the continuity of the salt section, significantly controls the later contractional deformation. This paper utilizes scaled sandbox models to analyse the interplay between sub-salt structures and supra-salt units during both extension and inversion. Series 1 experiments involved baseline models run using isotropic sand packs for simple and ramp-flat listric faults, as well as for simple planar and kinked planar faults. Series 2 experiments involved the same fault geometries but also included a pre-extension polymer layer to simulate salt in the stratigraphy. In these experiments, the polymer layer decoupled the extensional and contractional strains, and inhibited the upwards propagation of sub-polymer faults. In all Series 2 experiments, the extension produced a synclinal hanging-wall basin above the polymer layer as a result of polymer migration during the deformation. During inversion, the supra-polymer synclinal basin was uplifted, folded and detached above the polymer layer. Changes in thickness of the polymer layer during the inversion produced primary welds and these permitted the sub-polymer deformation to propagate upwards into the supra-salt layers. The experimental results are compared with examples from the Parentis Basin (Bay of Biscay), the Broad Fourteens Basin (southern North Sea), the Feda Graben (central North Sea) and the Cameros Basin (Iberian Range, Spain).
Pore-pressure prediction challenges in chemical compaction regimes: An alternative V P / V S -based approach
Characterization of the Devonian Kharyaga carbonate platform (Russia): Integrated and multiscale approach
Diapiric shale and coast-perpendicular, fault-related subbasins, south Texas Gulf Coast
Thin‐ or Thick‐Skinned Faulting in the Yakima Fold and Thrust Belt (WA)? Constraints from Kinematic Modeling of the Saddle Mountains Anticline
The Mineral, Virginia (USA), earthquake of 23 August 2011 occurred at 6–8 km depth within the allochthonous terranes of the Appalachian Piedmont Province, rupturing an ~N36°E striking reverse fault dipping ~50° southeast. This study used the Interstate Highway 64 seismic reflection profile acquired ~6 km southwest of the hypocenter to examine the structural setting of the earthquake. The profile shows that the 2011 earthquake and its aftershocks are almost entirely within the early Paleozoic Chopawamsic volcanic arc terrane, which is bounded by listric thrust faults dipping 30°–40° southeast that sole out into an ~2-km-thick, strongly reflective zone at 7–12 km depth. Reflectors above and below the southward projection of the 2011 earthquake focal plane do not show evidence for large displacement, and the updip projection of the fault plane does not match either the location or trend of a previously mapped fault or lithologic boundary. The 2011 earthquake thus does not appear to be a simple reactivation of a known Paleozoic thrust fault or a major Mesozoic rift basin-boundary fault. The fault that ruptured appears to be a new fault, a fault with only minor displacement, or to not extend the ~3 km from the aftershock zone to the seismic profile. Although the Paleozoic structures appear to influence the general distribution of seismicity in the area, Central Virginia seismic zone earthquakes have yet to be tied directly to specific fault systems mapped at the surface or imaged on seismic profiles.