Exemplos de uso de Passive margin em Inglês e suas traduções para o Português
{-}
-
Colloquial
-
Official
-
Medicine
-
Financial
-
Ecclesiastic
-
Ecclesiastic
-
Computer
-
Official/political
Sediment-starved margins produce narrow continental shelves and passive margins.
The pelotas basin is the classical example of a volcanic passive margin displaying large wedges of seaward-dipping reflectors sdr.
The edges of continental fragments formed this way(both sides of the Atlantic Ocean, for example)are termed passive margins.
The espírito santo basin is characterized as passive margin. it is formed during the separation between the south american and african continents in the fragmentation of gondwana.
Those results are similar for those found for the canastra group,which is commonly interpreted as part of the são francisco paleocontinent western passive margin.
The jequitinhonha basin has great geological complexity:a rift basin that evolved into passive margin with occurrence of magmatism and halokinesis.
The campos basin is a passive margin basin located at the southeastern brazilian coast, limited by the cabo frio high to the south, and by the vitoria high to the north.
The interpretation of ultra-deep seismic lines showed a very different geology from the adjacent santos, campos andespírito santo basins, which constitute examples of magma-poor passive margins.
The serra do mar is configured as a typical mature high-elevation passive margin, marking the event of separation between africa and south america and the formation of the south atlantic ocean.
The southern brasilia orogen has been interpreted as the result of the ediacaran collision between the active margin of the paranapanema plate and the passive margin of the são francisco paleocontinent.
It is believed that the sediments have been formed in a intracontinental rift progressing to passive margin, representing the beginning of a wilson cycle in the southern portion of the são francisco craton around 2.5 ga.
In the central portion of the south-america platform occurs the carbonate succession of the araras group, that register an extensive carbonate platforms of the neoproterozoic,developed along a passive margin at s-sw portion of the amazon craton.
The evolutionary dynamics of continental passive margins has been the subject of discussion in the global tectonics scope and the eastern south america margin comprises a number of marginal basins containing sedimentary records of several development stages of the coastal zone after the opening of the atlantic ocean.
The northern paraguay belt consists mainly of metasedimentary rocks of the cuiabá group(720 my.), assigned to passive margins basins in an extensional context during the break-up of supercontinent rodinia 1.0 gy.
Ages obtained indicate that the onset of sedimentation of the passo feio basin had as main source the paleoproterozoic and archean rocks of the rio de la plata craton and adjacent,at this time featuring a passive margin basin.
This type of tectonics is found at zones of continental collision, at restraining bends in strike-slip faults, andat the oceanward part of passive margin sequences where a detachment layer is present.
The continental rifted system that initiated in the late jurassic in southern argentina andevolved during the early cretaceous in the brazilian eastern margin heralded the gondwana break up and the formation of the south atlantic divergent passive margin.
The andrelândia nappe system(ans) is an important component of the neoproterozoic southern brasília orogen(sbo) in se brazil and its evolution is related to the convergence andsubsequent collision between the passive margin of the são francisco paleocontinent and paranapanema block during the brasiliano orogeny.
This type of tectonics is found at divergent plate boundaries, in continental rifts, during and after a period of continental collision caused by the lateral spreading of the thickened crust formed, at releasing bends in strike-slip faults,in back-arc basins, and on the continental end of passive margin sequences where a detachment layer is present.
The Gulf of Lion is not a simple passive continental margin; it results from Oligocene-Miocene anti-clockwise rotation of the Corsican-Sardinian Block against the European Craton.
Frade field is located in the campos basin approximately 115 km from the state of rio de janeiro coast in the south-central portion of the brazilian passive continental margin and has produced from oligocene and miocene turbidite reservoirs since 2009.
Recent endogenous processes provide dynamic movements in the lithosphere and generate the varied forms of relief,even in areas of passive continental margins, such as the research area of this work located in northeastern brazil.