rift basin वाक्य
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- Following the Gondwanide orogeny southwestern Gondwana entered a period of extensional tectonics and crustal thinning leading to formation of various rift basins ( e . g.
- Widely faulted and moderately rotated Upper Triassic to Lower Cretaceous beds within the rift basin were subsequently buried beneath a relatively unstructured cover of Upper Cretaceous and Tertiary strata.
- The crust was thinned in areas of stretching and the synchronous growth of faults allowed those areas to subside; that is, to sink relative to surrounding areas, thereby creating rift basins.
- This basin is one of a series of rift basins that are located on the broad, shallow promontory of continental crust known as the Grand Banks of Newfoundland off Canada's east coast.
- They are part of a massive " flood basalt " that underlies most of the Bay of Fundy, although the Grand Manan Basalt was later separated into its own rift basin by block faulting [ ref.
- More than 70 % of the mean undiscovered oil resources is estimated to occur in five provinces : Arctic Alaska, Amerasia Basin, East Greenland Rift Basins, East Barents Basins, and West Greenland East Canada.
- This magmatism led to the extrusion of abundant volcanic successions such as the Northeast German Basin, Northwest Polish Basin, and Oslo Rift, while also causing the formation of 70 rift basins throughout the Permian Basin.
- The Rockall Basin forms part of a chain of highly extended Mesozoic rift basins between the Charlie-Gibb and Senja Fracture Zones, that includes; the Faeroe-Shetland Basin, the M�re Basin, and the V�ring Basin.
- The West Baram fault runs northwest-southeast off the coast of Sarawak, Borneo and separates blocks of differing geological histories, one of which is the 2 ) The Continental Rift Basin Model where the line with triangles represents subduction.
- Extensional geological settings like the foreland basin and rift basin settings are found, Zigui Basin and Danyang Basin, which are the two sedimentary basins lying on the western and eastern flank of Huangling dome, were formed during Late Triassic and Jurassic.
- The technique developed by Watts & Ryan in 1976 allows for the recovery of the basement subsidence and uplift history in the absence of sediment and water loading and, therefore isolate the contribution from the tectonic forces responsible for the formation of a rift basin.
- The Late Paleocene to the Early Eocene ( 55 Ma ) saw rift basin formation in the Fuegan Andes which led to crustal extension : the first sign of separation between the two continents and the formation of the South Scotia Sea and South Scotia Ridge.
- The coal from this small pit was used to fuel his blacksmith shop on the same property . " Farmville has coal deposits because it sits on the Farmville Basin, one of the Eastern North America Rift Basins west of modern day, Virginia State Route 45.
- The basin originated as a rift basin in the context of extensional tectonics and crustal thinning that followed the Paleozoic Gondwanide orogeny . { { refn | name = note 1 | group = note | These tectonics are not related to the break-up of Gondwana later in the Mesozoic.
- The Gulf is underlain by the Gulf of California Rift Zone, a series of rift basins and transform fault segments between the northern end of the East Pacific Rise in the mouth of the gulf to the San Andreas Fault system in the vicinity of the Salton Trough rift / Brawley seismic zone.
- As the Jeanne d'Arc rift basin subsided, it was gradually in-filled with sediments eroded from adjacent areas of crustal uplift . Characteristics of the sedimentary basin fill and their relationships to the extensional history of the Jeanne d'Arc Basin have been variably described by numerous authors with general agreement on the applicability of rift concepts to the basin.
- The "'Niger Delta Basin "', also referred to as the "'Niger Delta province "', is an extensional rift basin located in the Niger Delta and the Gulf of Guinea on the passive continental margin near the western coast of Nigeria with suspected or proven access to Cameroon, Equatorial Guinea and S�o Tom?and Pr�ncipe.
- The Ramapo Fault, which marks the western boundary of the Newark rift basin, has been argued to be a major seismically active feature of this region, but it is difficult to discern the extent to which the Ramapo fault ( or any other specific mapped fault in the area ) might be any more of a source of future earthquakes than any other parts of the region.
- अधिक वाक्य: 1 2
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