rifted passive margin oor Frans
rifted passive margin
Vertalings in die woordeboek Engels - Frans
marge passive de divergence
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
This created the rifted passive margins of the Atlantic and established the tectonic and climatic setting of wrench-generated coastal ranges and detrital basins bordering vast salt flats that were overlain with waters from the Tethys Sea.
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Further, we interpret the lower MRS (Chocolay Group), a glaciogenic and shallow-marine succession that lies atop Archean basement, to be equivalent to the upper part of the Huronian Supergroup of Ontario and to represent the original continental rifting and passive-margin phase of the Penokean cycle.
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Structural–stratigraphic relationships indicate that the loci of the dykes are controlled by Helikian to Upper Paleozoic extensional fault systems associated with rifting of the ancestral passive margin.
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This external zone corresponds to the internal part of the European passive margin developed during Liassic rifting.
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The ancient Laurentian margin rifted in the latest Neoproterozoic to early Cambrian but appears not to have developed as a simple passive margin through a long, post-rift, drift phase.
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But in Middle Jurassic times, 175 million years ago, Pangea began to rift apart, and North America’s passive western margin became active.
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Rifting and continental breakup result in unique sediment sequences on passive margins.
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Successive lithotectonic units reflecting evolution of the tectonic framework include pre-Appalachian crystalline basement, rift-fill sedimentary and volcanic rocks, passive-margin shelf and off-shelf facies, and synorogenic clastic wedges.
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These features are inferred to represent passive-margin sediments deposited on the ancient rifted margin during the mid-to-late Proterozoic and early Paleozoic.
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The first sequence records 2.17 Ga rifting and the development, by 2.14 Ga, of a passive margin along the eastern part of the Superior craton.
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The Gödene Zone, Antalya Complex, is an assemblage of ophiolitic and associated sedimentary rocks formed on a passive margin during and after the rifting of a Mesozoic ocean basin.
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It is suggested that in the upper Ordovician there existed on the one hand a passive continental margin or continental rift flooded by the sea, where mildly-alkaline basalts erupted (Magdalensberg-Series/Carinthia; Kaser-Series/Gurktaler Alpen).
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The second Neoproterozoic rifting (Hamill–Gog) is interpreted to indicate continental breakup and establishment of a passive margin along western Laurentia.
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Instead, Windermere sedimentation occurred as a result of a protracted, episodic rift history that culminated with latest Proterozoic – Early Cambrian rifting associated with the onset of thermal subsidence in the ancient passive margin.
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The earlier Neoproterozoic (Windermere-age) rifting event probably records breakup of a continental mass from northern Laurentia followed by development of a passive margin.
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The Lower Cambrian McNaughton Formation of the Gog Group occupies a stratigraphic position transitional between the rift-related rocks of the underlying Upper Proterozoic Miette Group, and the overlying Paleozoic passive margin succession.
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Moreover, the Hamill Group contains the sedimentological record of the passage of the ancient passive margin from unstable tectonic conditions associated with rifting and (or) the earliest phases of thermal subsidence to post-rift conditions characterized by stabilization of the margin and dissipation of the thermal anomaly generated during the rift phase (the rift to post-rift transition).
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The passive margin that existed in northern Laurentia during the early Paleozoic was, therefore, established in the late Neoproterozoic, and the onset of rifting must have preceded this, rather than occurring in the Early Cambrian as some authors have suggested.
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Rifting and continental breakup result in unique sediment sequences on passive margins. The initial rift valleys were probably occupied by stratified fresh water lakes due to the equable Mesozoic climate, and during this phase might have accumulated about 7.5×1021 g of organic carbon; this would be 14% of the earth's total organic carbon concentrated on only 0.3% of the earth's surface.
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Rapid subsidence, initiated by rifting in the Carboniferous and Early Permian, was followed by thermal subsidence at a more sedate rate, in passive margin fashion.
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Spatial and chronological transition from an orogenic belt to a passive margin from the analyze of residual tectono-sedimentary markers preserved in the surrounding areas: example from the eastern pyreneene foreland (Languedoc, Provence, Lion Gulf). -What structures are generate in an orogen and preserved after the rifting period?
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21 sinne gevind in 29 ms. Hulle kom uit baie bronne en word nie nagegaan nie.