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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa (1)
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East Africa
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Kenya (1)
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Sudan (1)
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East African Rift (2)
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Libya
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Sahara (4)
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Southern Africa
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Volta Basin (1)
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West Africa
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geologic age
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Tertiary
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Dongying Formation (1)
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lower Eocene (1)
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Hanna Formation (1)
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Paleozoic
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Carboniferous
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Primary terms
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absolute age (12)
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Africa
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East Africa
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Kenya (1)
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East African Rift (2)
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Algeria
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Ghadames Basin (2)
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Illizi Basin (1)
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Libya
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Sirte Basin (1)
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Tunisia (1)
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Sahara (4)
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Southern Africa
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Kaapvaal Craton (1)
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Namaqualand (1)
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Namibia
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Damara Belt (1)
-
-
-
Volta Basin (1)
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West Africa
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Cameroon (1)
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Chad (1)
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Ghana (1)
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Gujarat India (1)
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Bokaro coal field (1)
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Pranhita-Godavari Valley (1)
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Singhbhum shear zone (1)
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Middle East (1)
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Tyumen Russian Federation
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Vindhyan Basin (2)
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West Siberia
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Siberian Lowland (2)
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Atlantic Ocean
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North Atlantic
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Hudson Bay (1)
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North Sea
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Brent Field (1)
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Oseberg Field (1)
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Statfjord Field (1)
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Viking Graben (1)
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South Atlantic
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Cape Basin (1)
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Walvis Ridge (1)
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Atlantic Ocean Islands
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Tristan da Cunha (1)
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Australasia
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Australia
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barite deposits (1)
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Canada
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Nunavut
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Western Canada
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carbon
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Cenozoic
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Quaternary
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Holocene (1)
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Tertiary
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Neogene
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Miocene (2)
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Paleogene
-
Dongying Formation (1)
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Eocene
-
lower Eocene (1)
-
-
Hanna Formation (1)
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Oligocene (2)
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Paleocene
-
Ravenscrag Formation (1)
-
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Chordata
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Vertebrata (1)
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clay mineralogy (2)
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continental drift (1)
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continental shelf (1)
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crust (11)
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data processing (2)
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Deep Sea Drilling Project
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IPOD
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Leg 75
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DSDP Site 530 (1)
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Leg 40
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intracratonic basins
Hypogenic karstic cavities formed by tectonic-driven fluid mixing in the Ordovician carbonates from the Tarim Basin, northwestern China
Tectonics of the Paleoproterozoic Rinkian orogen, central West Greenland
3D numerical modelling and simulation of the impact of fault zones on fluid flow in sandstones of the Rio do Peixe Basin, NE Brazil
Fine-Scale Three-Dimensional Characterization of a Reservoir Comprising Braided River Sand Bodies with a Complex Stacking Pattern in a Cratonic Basin
Palaeosedimentary Environment and Formation Mechanism of High-Quality Xujiahe Source Rocks, Sichuan Basin, South China
The initiation of the Mesoproterozoic Bylot basins (Nunavut, Arctic Canada) as recorded in the Nyeboe Formation, Fury and Hecla Group
Gravimetry and petrophysics for defining the intracratonic and rift basins of the Western-Central Africa zone
West Texas (Permian) Super Basin, United States: Tectonics, structural development, sedimentation, petroleum systems, and hydrocarbon reserves
So close and yet so far: U–Pb geochronological constraints of the Jaibaras Rift Basin and the intracratonic Parnaíba Basin in SW Gondwana
Control of inherited accreted lithospheric heterogeneity on the architecture and the low, long-term subsidence rate of intracratonic basins
Pore Characteristics of Gondwana Shale of Eastern India
Classification of the Paleoproterozoic Gulcheru Formation: Implications on Early Paleogeographic and Tectonic Evolution of the Cuddapah Basin, India
Late Paleozoic detrital history of eastern Gondwanaland: petrofacies and detrital geochronology of Permo-Carboniferous intracratonic sequences of the northwest Bengal Basin
Thermal history of potential gas reservoir rocks in the eastern Parnaíba Basin, Brazil
Fault-related overpressure in the Krishna-Godavari Basin, India
Abstract Sub-ophitic, equigranular or plagioclase-phyric dolerite dykes, referred to as the Blekinge–Dalarna dolerite (BDD) swarm, were emplaced during the time span 0.98–0.95 Ga and trend NNE–NNW in an arcuate fashion, parallel to and east of the Sveconorwegian orogen. Dolerite sills are locally present. These rocks are subalkaline to alkaline with a monzogabbroic or gabbroic composition and show a predominantly within-plate tectonic affinity. ɛ Nd and ɛ Hf values fall in the range −2 to +4 and +1 to +5, respectively. Siliciclastic sedimentary rocks (Almesåkra Group) in a small outlier in southern Sweden were deposited in an aeolian to fluviatile or lacustrine environment and an arid or semi-arid warm palaeoclimate, coevally with the dolerite sills. Smaller occurrences of sandstone with peperitic field relationships to the BDD dykes are known from other localities. The spatial distribution, orientation and age of the BDD magmatic suite suggest roughly east–west extension in the eastern, cratonic foreland to the Sveconorwegian orogen during the latest phase of this mountain-building event, the age data tentatively suggesting a younging to the east. The siliciclastic sedimentary rocks represent an erosional relict of a larger and spatially much more extensive early Tonian foreland basin to this orogen, as proposed earlier on the basis of fission-track thermochronology.