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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Gulf of Saint Lawrence (7)
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-
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Atlantic region (1)
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Australasia
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Australia
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Queensland Australia
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Burdekin River (1)
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Avalon Zone (1)
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Canada
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Eastern Canada
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Maritime Provinces
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New Brunswick
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Gloucester County New Brunswick (1)
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Moncton Basin (3)
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Nova Scotia
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Cape Breton Island (8)
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Cobequid Highlands (1)
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Cumberland County Nova Scotia (2)
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Gays River Deposit (5)
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Pictou County Nova Scotia (1)
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Meguma Terrane (2)
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Newfoundland and Labrador
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Newfoundland
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Quebec
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Cumberland Basin (4)
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Europe
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Western Europe
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Maritimes Basin (42)
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North America
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Appalachians
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Canadian Shield
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Grenville Province (2)
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Humber Zone (1)
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Southern Hemisphere (1)
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Sydney Basin (3)
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United States
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North Carolina (1)
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South Carolina (1)
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White Bay (1)
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commodities
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barite deposits (5)
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bitumens (3)
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brines (10)
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metal ores
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base metals (4)
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copper ores (3)
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lead ores (1)
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lead-zinc deposits (10)
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silver ores (2)
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mineral deposits, genesis (6)
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mineral exploration (1)
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mineral resources (1)
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petroleum
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natural gas
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coalbed methane (1)
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elements, isotopes
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carbon
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C-13/C-12 (4)
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organic carbon (1)
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chemical ratios (1)
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hydrogen
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D/H (1)
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isotope ratios (6)
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Rb-87/Sr-86 (1)
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Sm-147/Nd-144 (1)
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stable isotopes
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C-13/C-12 (4)
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D/H (1)
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Nd-144/Nd-143 (1)
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O-18/O-16 (4)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Rb-87/Sr-86 (1)
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S-34/S-32 (3)
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Sm-147/Nd-144 (1)
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Sr-87/Sr-86 (4)
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metals
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alkali metals
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rubidium
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Rb-87/Sr-86 (1)
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sodium (1)
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alkaline earth metals
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calcium (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (4)
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-
lead
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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rare earths
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neodymium
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Nd-144/Nd-143 (1)
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Sm-147/Nd-144 (1)
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samarium
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Sm-147/Nd-144 (1)
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oxygen
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O-18/O-16 (4)
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sulfur
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S-34/S-32 (3)
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fossils
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Chordata
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Vertebrata (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Ostracoda (1)
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Trilobitomorpha
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Trilobita (1)
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Brachiopoda (1)
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Cnidaria
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Anthozoa
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Rugosa (1)
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Protista
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Foraminifera (2)
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microfossils
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Conodonta (1)
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palynomorphs
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miospores
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pollen (1)
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Plantae
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algae (1)
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Pteridophyta
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Lycopsida (1)
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geochronology methods
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fission-track dating (1)
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paleomagnetism (2)
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geologic age
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Cenozoic
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Tertiary
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Paleogene (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Barremian (1)
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Jurassic (1)
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Paleozoic
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Carboniferous
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Albert Formation (2)
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Lower Carboniferous
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Asbian (1)
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Dinantian (13)
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Mabou Group (5)
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Mississippian
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Lower Mississippian
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Tournaisian (3)
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Macumber Formation (6)
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Middle Mississippian
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Visean
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upper Visean (1)
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Upper Mississippian (1)
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Windsor Group (15)
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Namurian (1)
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Pennsylvanian
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Cumberland Group (5)
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Joggins Formation (2)
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Lower Pennsylvanian (1)
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Morien Group (2)
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Upper Carboniferous
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Westphalian (1)
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Devonian
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Upper Devonian (1)
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Horton Group (10)
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middle Paleozoic (1)
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Ordovician (2)
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Permian
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Lower Permian (1)
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Silurian (1)
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upper Paleozoic
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Kiaman Superchron (1)
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Pictou Group (3)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (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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volcanic rocks
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basalts
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mid-ocean ridge basalts (1)
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ocean-island basalts (1)
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tholeiitic basalt (1)
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pyroclastics
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tuff (1)
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metamorphic rocks
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minerals
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phosphates
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silicates
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clay minerals
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smectite (1)
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illite (1)
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sulfates
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barite (1)
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sulfides
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sphalerite (1)
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Primary terms
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Atlantic Ocean
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North Atlantic
-
Gulf of Saint Lawrence (7)
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-
-
Atlantic region (1)
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Australasia
-
Australia
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Queensland Australia
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Burdekin River (1)
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-
-
-
barite deposits (5)
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biogeography (1)
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bitumens (3)
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brines (10)
-
Canada
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Eastern Canada
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Maritime Provinces
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New Brunswick
-
Gloucester County New Brunswick (1)
-
Moncton Basin (3)
-
-
Nova Scotia
-
Cape Breton Island (8)
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Cobequid Highlands (1)
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Cumberland County Nova Scotia (2)
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Gays River Deposit (5)
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Pictou County Nova Scotia (1)
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-
-
Meguma Terrane (2)
-
Newfoundland and Labrador
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Newfoundland
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Great Northern Peninsula (1)
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Port au Port Peninsula (1)
-
-
-
Quebec
-
Anticosti Island (1)
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Magdalen Islands (1)
-
-
-
-
carbon
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C-13/C-12 (4)
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organic carbon (1)
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Cenozoic
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Tertiary
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Paleogene (1)
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Chordata
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Vertebrata (1)
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clay mineralogy (2)
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climate change (1)
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crust (1)
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deformation (4)
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diagenesis (4)
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economic geology (1)
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Europe
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faults (10)
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folds (4)
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foliation (1)
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geochronology (1)
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geophysical methods (7)
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glacial geology (1)
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ground water (2)
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heat flow (3)
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hydrogen
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D/H (1)
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hydrology (1)
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igneous rocks
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plutonic rocks
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granites (1)
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volcanic rocks
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basalts
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mid-ocean ridge basalts (1)
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ocean-island basalts (1)
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tholeiitic basalt (1)
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pyroclastics
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tuff (1)
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inclusions
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fluid inclusions (4)
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intrusions (2)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Ostracoda (1)
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-
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Trilobitomorpha
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Trilobita (1)
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Brachiopoda (1)
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Cnidaria
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Anthozoa
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Zoantharia
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Rugosa (1)
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-
-
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Protista
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Foraminifera (2)
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Rb-87/Sr-86 (1)
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Sm-147/Nd-144 (1)
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stable isotopes
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C-13/C-12 (4)
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D/H (1)
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Nd-144/Nd-143 (1)
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O-18/O-16 (4)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Rb-87/Sr-86 (1)
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S-34/S-32 (3)
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Sm-147/Nd-144 (1)
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Sr-87/Sr-86 (4)
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lineation (1)
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magmas (1)
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mantle (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Barremian (1)
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Jurassic (1)
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metal ores
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base metals (4)
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copper ores (3)
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lead ores (1)
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lead-zinc deposits (10)
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silver ores (2)
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zinc ores (1)
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metals
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alkali metals
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rubidium
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Rb-87/Sr-86 (1)
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sodium (1)
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alkaline earth metals
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calcium (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (4)
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lead
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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rare earths
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neodymium
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Nd-144/Nd-143 (1)
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Sm-147/Nd-144 (1)
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samarium
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Sm-147/Nd-144 (1)
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metamorphic rocks
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metaigneous rocks (1)
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mylonites (2)
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mineral deposits, genesis (6)
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mineral exploration (1)
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mineral resources (1)
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North America
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Appalachians
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Northern Appalachians (2)
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Canadian Shield
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Grenville Province (2)
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Humber Zone (1)
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orogeny (1)
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oxygen
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O-18/O-16 (4)
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paleoclimatology (4)
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paleogeography (5)
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paleomagnetism (2)
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Paleozoic
-
Carboniferous
-
Albert Formation (2)
-
Lower Carboniferous
-
Asbian (1)
-
Dinantian (13)
-
-
Mabou Group (5)
-
Mississippian
-
Lower Mississippian
-
Tournaisian (3)
-
-
Macumber Formation (6)
-
Middle Mississippian
-
Visean
-
upper Visean (1)
-
-
-
Upper Mississippian (1)
-
Windsor Group (15)
-
-
Namurian (1)
-
Pennsylvanian
-
Cumberland Group (5)
-
Joggins Formation (2)
-
Lower Pennsylvanian (1)
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Morien Group (2)
-
-
Upper Carboniferous
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Westphalian (1)
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-
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Devonian
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Upper Devonian (1)
-
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Horton Group (10)
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middle Paleozoic (1)
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Ordovician (2)
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Permian
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Lower Permian (1)
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-
Silurian (1)
-
upper Paleozoic
-
Kiaman Superchron (1)
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Pictou Group (3)
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palynomorphs
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miospores
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pollen (1)
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paragenesis (5)
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petroleum
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natural gas
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coalbed methane (1)
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Plantae
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algae (1)
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Pteridophyta
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Lycopsida (1)
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plate tectonics (2)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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sea-floor spreading (1)
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sea-level changes (4)
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sedimentary petrology (2)
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sedimentary rocks
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chemically precipitated rocks
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clastic rocks
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conglomerate (2)
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siltstone (1)
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coal (2)
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sedimentary structures
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bedding plane irregularities
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planar bedding structures
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soft sediment deformation
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clastic dikes (1)
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sedimentation (4)
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sediments (1)
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Southern Hemisphere (1)
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stratigraphy (2)
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structural analysis (2)
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structural geology (1)
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sulfur
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S-34/S-32 (3)
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tectonics
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salt tectonics (5)
-
-
United States
-
North Carolina (1)
-
South Carolina (1)
-
-
-
rock formations
-
Deer Lake Group (1)
-
-
sedimentary rocks
-
sedimentary rocks
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carbonate rocks
-
boundstone (1)
-
dolostone (1)
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limestone (1)
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packstone (1)
-
wackestone (1)
-
-
chemically precipitated rocks
-
evaporites (5)
-
-
clastic rocks
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conglomerate (2)
-
mudstone (2)
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sandstone (5)
-
shale (1)
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siltstone (1)
-
-
coal (2)
-
-
-
sedimentary structures
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boudinage (1)
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channels (2)
-
sedimentary structures
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bedding plane irregularities
-
flute casts (1)
-
-
planar bedding structures
-
cyclothems (1)
-
-
soft sediment deformation
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clastic dikes (1)
-
-
-
-
sediments
-
sediments (1)
-
-
soils
-
paleosols (1)
-
Maritimes Basin
Paleotethyan faunal/floral evidence in the Mississippian Maritimes Basin of Canada: An overview
The northern Appalachian terrane wreck model
Sequence stratigraphy of the late Carboniferous Clifton Formation, New Brunswick
The Upper Visean Magdalen Islands Basalts of Eastern Quebec, Canada: A Complex Assemblage of Contrasting Mafic Rock Types Erupted in Peak Stages of Transtensional Basin Development above a Mantle Plume
Statistical analysis of forward stratigraphic models in complex salt provinces: The central Scotian Basin case study
Magnetic polarity stratigraphy and palynostratigraphy of the Mississippian-Pennsylvanian boundary interval in eastern North America and the age of the beginning of the Kiaman
Deconvolving Signals of Tectonic and Climatic Controls From Continental Basins: An Example From the Late Paleozoic Cumberland Basin, Atlantic Canada
Evaporite tectonics and the late Paleozoic stratigraphic development of the Cumberland basin, Appalachians of Atlantic Canada
Fluvial response to paleo-equatorial climate fluctuations during the late Paleozoic ice age
Geological setting and resource potential of conventional petroleum plays in Paleozoic basins in eastern Canada
Overstep and imbrication along a sidewall ramp and its relationship to a hydrocarbon play in Tournaisian rocks of the Moncton Basin: the Peck Creek section, Albert Mines area, southeastern New Brunswick
Kennetcook thrust system: late Paleozoic transpression near the southern margin of the Maritimes Basin, Nova Scotia
Facies model for fluvial systems in the seasonal tropics and subtropics
Truncation and translation of Appalachian promontories: Mid-Paleozoic strike-slip tectonics and basin initiation
In paleoequatorial parts of Europe and North America, late Paleozoic cyclic successions are widely inferred to reflect glacio-eustasy. However, many of these successions accumulated in basins in the Pangean collisional zone, where variations in tectonics and sediment supply could also have generated cyclic successions. Cyclic successions are ubiquitous in the Maritimes Basin of Atlantic Canada but are especially prominent in the Visean and Bolsovian to Cantabrian, when subsidence rates on coastal plains were low and probably steady during periods of thermal subsidence. During relatively humid climatic conditions in the Bolsovian to Cantabrian, fluvial systems generated clastic cyclic successions with deep valleys and mature interfluve paleosols, providing strong evidence for alternate rise and fall of sea level—a characteristic glacio-eustatic feature. Under arid conditions in the Visean, with few rivers, carbonate-evaporite rhythms formed with little evidence for incision. Comparisons with near- and far-field records for Gondwanan glacial activity suggest that these two periods correspond to sea-level changes on the order of a few tens of meters, probably due to melting and accumulation of small ice caps rather than continent-wide ice sheets. Cyclic successions that formed in basins undergoing steady thermal subsidence may provide the most reliable evidence for glacio-eustasy in the paleoequatorial realm.