back-arc marginal basin
bassin marginal d'arrière-arc
back arc basin oor Frans
back arc basin
Vertalings in die woordeboek Engels - Frans
bassin arrière-arc
bassin d'arrière-arc
Lower Cretaceous sequences in the west and east may represent a volcanic arc and back-arc basin.
Les séquences du Crétacé inférieur dans l'ouest et l'est peuvent représenter un arc volcanique et un bassin d'arrière-arc.
bassin intra-arc
bassin marginal
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
Soortgelyke frases
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
Lower Cretaceous sequences in the west and east may represent a volcanic arc and back-arc basin.
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By 1.19 Ga the Elzevir back arc basin was closing.
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Co-Chairman of the working group on back-arc basins of the inter-ridge (since 1997)
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Eastward subduction of the KMA beneath ancient North America collapsed the back-arc basin by latest Cretaceous time.
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The Cuzco-Sicuam Basin, Maestrichtian-Paleocene in age, is a back-arc basin.
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It formed by subduction and back-arc basin opening and closure during the Silurian to Early Devonian.
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A compatible tectonic setting is a back-arc basin within influence of a continental source.
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Hydrothermal vents are found on active spreading ridges, in subduction zones, fracture zones, back-arc basins and on seamounts
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Hydrothermal vents are found on active spreading ridges, in subduction zones, fracture zones, back-arc basins and on seamounts.
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The Slide Mountain Terrane is considered to represent a back-arc basin related to the Quesnellia Paleozoic arc-terrane.
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The early thrusting records the closure of a back-arc basin within the Central Metasedimentary Belt, which closed at ca.
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The Ordovician–Silurian rocks of the Aspy "terrane" are interpreted to have formed in an arc–back-arc basin system.
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The supracrustal rocks may have been deposited in a back-arc basin floored at least in part by attenuated continental material.
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This supports a model in which thrust slices juxtapose remnants of volcanic centres erupted at different locationswithin a back-arc basin.
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Volcanics and granitic rocks have immobile-element geochemical affinities with volcanics from continental-margin-arc systems and associated back-arc basins.
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Additional extensional movements were related to the formation of the Aegean back arc basin caused by the Late Cenozoic Hellenic subduction zone.
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The upper unit indicates major changes to a back-arc basin linked to the Ottarasko, and possibly Gambier, arc to the west.
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The oceanic back-arc-basin igneous rocks form the basement to renewed arc-related basaltic volcanism in late Middle to Late Ordovician time.
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The Taylor Creek Group (Albian) is the first definitive link between the two belts and represents an arc and intra-arc or back-arc basin.
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The back-arc-basin setting appears to be ensialic and is characterized by the absence of an underlying subducted slab during the formation of the basin.
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Around 1.25 Ga, the geological record is dominated by dyke-swarm intrusion, continental rift basin formation, A-type felsic magmatism, and arc – back-arc basin development.
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The Burnt Lake back-arc tholeiitic suite comprises basalts similar in trace element signature to tholeiitic basalts emplaced in back-arc basins formed in continental crust.
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An ocean-island component is involved in the back-arc related petrogenetic processes, producing magmas with compositions intermediate between arc tholeiites and enriched back-arc basin basalts.
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The felsic magmatism and VMS deposits likely formed in an Okinawa-type back-arc basin developed from rifting the Early Ordovician Popelogan continentalarc, of which the southern plutons are remnants.
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Hydrothermal processes in back-arc basins (BABs), a special type of sub-marine basin, generate a rich variety of vent chemistry and mineral deposits and therefore, chemical exchanges are important here.
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