stage of rifting
stade de distension · stade de rifting
rifting stage oor Frans
rifting stage
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stade de distension
stade de rifting
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Greenland was formed in two rifting stages from the main body of North America.
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An initial rift stage in the Early Jurassic is characterized by normal–oblique faults bounding tilted blocks, which are associated with tensional paleostress patterns whose minimum component trends west-northwest–east-southeast.
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Based on the model that during the rifting stage beginning at ca. 590 Ma, the Ottawa Graben, an Iapetan failed arm, localized a large river that flowed into the nascent Iapetus, a search was made for the related fluvial and deltaic deposits.
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The slope of this curve depends upon the temperature to which the crust and upper mantle were heated during the initial rifting stage and can be used to derive the temperature–time history within the sediments, the present temperature distribution, and geothermal gradient.
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Thus, a rift stage (Permian to Early Jurassic) in the tectonic history of the Western High Atlas was followed by a gulf stage (Late Jurassic to Middle Cretaceous) until later the high mountain range generated by inversion in Late Cretaceous and Neogene to recent times.
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Subsidence associated with the rifting and cooling stages of rifted margin formation was calculated from gridded maps of sediment thickness and bathymetry along the Labrador, Grand Banks, and Nova Scotian margins.
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These faults represent the final stage of rifting on the continental margin.
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The presence of longitudinal faults which control both the locations of mineralization and younger grabben fill volcanic sequences indicate late stage rifting during the development of the arc.
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The formation and subsequent alteration of iron, manganese and sulfide skarn ores in the Supracrustal Series involve: (1) late Initial Rift Stage exhalative-sedimentary processes possibly related to ascending granitic magma, (2) early Rift Stage exhalative-sedimentary and seafloor hydrothermal processes related to basic volcanism and intrusion and subvolcanic granite intrusion, (3) late Rift Stage hydrothermal metasomatic alteration and mineralization around subvolcanic granites, (4) Post-rift Stage deformation and metamorphism, (5) Post-rift Stage post-deformation recrystallization and skarn formation related to Hyttsjö diorites, and (6) post-Supracrustal Series metamorphic modifications.
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A later stage of rifting (Middle Jurassic) is characterized by large normal faults and is supposed to accompany local movements, probably due to gravity.
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A northwest system of dikes and faults indicated by the shaded relief map may be related to later stages of Keweenawan rifting.
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Continental rift systems and their possible stages of development are directly related to the split up of continents and the corresponding movements.
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The Caldwell basalts erupted in the final stages of Iapetus rifting, when the predominant mantle source involved in melting was the depleted asthenosphere.
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The transatlantic rift over the next stage of the war - specifically the implications of American policies with respect to the "axis of evil" - will not be easily resolved, to put it mildly.
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Strata of the Kennedy Channel Formation reflect repeated progradation of shallow-water facies into a slowly subsiding basin that developed in response to subsidence at a late stage of rift development along the Franklinian shelf margin.
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The dike composition differs from that of known Late Triassic and Early Jurassic continental tholeiites nearby in Nova Scotia, which are associated with a late stage of continental rifting.
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During the initial stage the Atlas-Rift and the Atlantic furrow were part of the global fracture zone, along which Pangea began to break up in post-Variscan time.
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From these new age results, it is now possible to expand the known distribution of Geon 15 magmatism in the region, confirm an early stage of Midcontinent Rift mafic magmatism between 1150 and 1130 Ma, provide evidence that significant mafic–ultramafic magmatism occurred in the Lake Nipigon region slightly earlier (~1115–1110 Ma) than the main stage of rift magmatism (1108–1094 Ma), and further document synchronous ~1110–1100 Ma tholeiitic and alkaline magmatism.
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Basin initiation may have been related to extensional tectonics, possibly on rifted continental crust, whereas later stages of basin history were characterized by compression, suggesting a foreland or fore-arc basin setting.
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The apparent contrast between the tectonic environment and the type of magmas erupted in the Anisian-Carnian is tentatively explained by partial melting during the early stage of rifting of an upper mantle deeply modified during the previous Hercynian orogenesis and contaminated by crustal material.
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All the above stages are recognizable along the Afro-Arabian Rifts and seem to have morphological equivalents in the Atlantic.
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The whole suite appears to have been formed in one series of related events, developing a rifted ensialic environment at a late stage in the evolution of the Slave craton.
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The main structures inherited from the rifting stage are reactiviated during a post-rift uplift of the margins.
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New data on the Atlantic rifting stage in the western Pyrenees during the Kimmeridgian: the Ouzous slump (Hautes-Pyrénées Auteurs:
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Ignorance of the vertical motions of the lithosphere induced by late-stage compression during post-rift evolution can, therefore, give rise to substantial errors in the estimates of crustal extension derived from analysis of basement subsidence using stretching models.
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72 sinne gevind in 17 ms. Hulle kom uit baie bronne en word nie nagegaan nie.