Pliensbachian oor Frans
Pliensbachian
en
A subdivision of the Jurassic period.
Vertalings in die woordeboek Engels - Frans
Pliensbachien
en
a subdivision of the Jurassic period
The existence of this corridor during the Pliensbachian is supported by several lines of independent paleobiogeographic evidence.
L'existence de ce corridor durant le Pliensbachien est mise en évidence par plusieurs observations paléographiques indépendantes.
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
The Middle Lias (Pliensbachian) started off transgressive as well with fine-grained detrital, limey to marly sediments (ferruginous oolites, fossiliferous limestones and marls) that change over to marls.
Alors ils mourrontWikiMatrix WikiMatrix
In the eastern and central parts of N Switzerland, sediments Sinemurian in age constitute about 90% of the total thickness. To the West, however, in the Mont Terri area, Pliensbachian and Toarcian deposits form 70% of the total thickness.
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The Lower to Middle Jurassic (Pliensbachian to lower Bajocian) Spatsizi Group in the northern Spatsizi area of north-central British Columbia is formally defined and subdivided into the Joan, Wolf Den, Melisson, Abou, and Quock formations.
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The north to south climatic zonation of upper Pliensbachian ammonites known in Europe has been recognized in the North American Cordillera.
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The South American record is restricted to upper Pliensbachian to lower Toarcian occurrences, suggesting that the species originated in the northeast Pacific in late Sinemurian time and spread to the southeast Pacific by the late Pliensbachian.
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The existence of this corridor during the Pliensbachian is supported by several lines of independent paleobiogeographic evidence.
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Neosuchians first appear in the Early Jurassic with the earliest known goniopholid Calsoyasuchus, which lived during the Sinemurian and Pliensbachian stages.
Prends le volantWikiMatrix WikiMatrix
The amaltheids are restricted temporally to the late Pliensbachian and geographically to the northern part of the northern hemisphere.
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These strata are probably latest Pliensbachian in age (Spinatum Standard Zone; Early Jurassic) and are tentatively correlated with the Jaeger Formation.
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U–Pb dates of and 186 ± 1 Ma from a granite clast and tuff unit, respectively, of the Kunae Zone (early late Pliensbachian) and sandstone–conglomerate petrofacies indicate a late Pliensbachian depositional regime dominated by tectonic controls.
Motifs de la réexpéditionGiga-fren Giga-fren
The transgressive–regressive curve for the formations points to a strong tectonic influence, but the late Norian and late Hettangian regressions and early Sinemurian, early Pliensbachian, and early late Pliensbachian transgressions are consistent with inferred eustatic events.
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This study extends the age range of Limbicysta considerably (late Pliensbachian to early Santonian), and the geographic occurrence from the Southern Hemisphere into the Northern Hemisphere.
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The following ages were determined (with 2s errors): 194.0+9.1–1.8 Ma from the Plesechioceras? harbledownense Assemblage (upper Sinemurian), 191.5 ± 0.8 Ma from the Plesechioceras? harbledownense Assemblage (upper Sinemurian) to the Whiteavesi Zone (lower Pliensbachian), 185.6+6.1–0.6 Ma from the Freboldi Zone (lower Pliensbachian), 184.7 ± 0.9 Ma from the Kunae Zone (upper Pliensbachian), 180.4+8.0–0.4 Ma from the Kanense to Planulata zones (lower to middle Toarcian), 179.8 ± 6.3 Ma from the Yakounensis Zone (upper Toarcian) to the lower Bajocian, 167.2+10.5–0.4 Ma from the Rotundum Zone (upper Bajocian), 158.2+1.9–0.4 Ma from the upper Bathonian, and 162.6+2.9–7.0 from the upper Bathonian to lower Callovian.
• Conclusion généraleGiga-fren Giga-fren
The Sinemurian or late Sinemurian – early Pliensbachian ages are older than previously reported U–Pb and biostratigraphic ages for presumed correlative rocks to the west, and westward-migrating volcanism is implied.
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The influx of granitic detritus indicates a rapid transition to a fully dissected arc provenance, where accelerated uplift of segments of the arc massif, accompanied by intra-arc strike-slip faulting, resulted in rapid arc dissection and unroofing of comagmatic Pliensbachian plutons.
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With further documentation the amount of offset of these zones should provide a measure of the amount of movement on these faults since Pliensbachian time and further document the allochthoneity of the western part of the Cordillera.
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Diversification took place in the latest Pliensbachian (Spinatum Zone) and early Toarcian (Tenuicostatum Zone), whereas diversity decrease occurred in the middle early Toarcian (Strangewaysi Subzone, Serpentinus Zone).
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Seasonally dry climatic conditions were developed first in the northeastern region of the basin during the Pliensbachian, followed by basin-wide seasonal dryness during the Bajocian.
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The presence of Hettangian and lower Pliensbachian strata in outcrop of the Gordondale Member is confirmed.
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The extinction and recovery of Ostracoda at the Pliensbachian–Toarcian (P–T) boundary are analyzed based on a database of taxonomically revised Pliensbachian to Toarcian transition ostracod assemblages.
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Southwest-derived, northerly longitudinal paleoflow during the Sinemurian changed to opposed bidirectional radial or transverse paleoflow systems in the early Pliensbachian.
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During the early Pliensbachian, arc dissection was interrupted by a major magmatic episode with widespread rejuvenated volcanism that caused a strong provenance shift to volcanigenic sources, indicating derivation from a largely undissected Stikinian arc.
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The Chilliwack terrane of southwestern British Columbia is a Pliensbachian paleobiogeographic anomaly.
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Paleobiogeographic patterns on the major allochthonous terranes argue against terrane rotation and in support of post-Pliensbachian northward displacement relative to the North American craton.
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An extinction rate of 54% has been calculated for upper Pliensbachian ostracod species occurring in more than one section.
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53 sinne gevind in 6 ms. Hulle kom uit baie bronne en word nie nagegaan nie.