stratigraphic succession oor Frans

stratigraphic succession

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succession stratigraphique

Overall, the stratigraphic succession is that of continental sediments, primarily fluvial, eolian, and playa lacustrine facies.
Généralement, la succession stratigraphique est formée de sédiments continentaux, principalement de faciès fluviaux, éoliens et de playa lacustres.
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In the Phyllite Group of Crete a stratigraphic succession from Permian to Upper Triassic members is represented.
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Overall, the stratigraphic succession is that of continental sediments, primarily fluvial, eolian, and playa lacustrine facies.
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Laurentide deposits are of Late Wisconsinan age and are restricted to the uppermost part of the stratigraphic succession.
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Some details of the stratigraphical succession are given and a previously unrecorded development of Oligocene rocks is described.
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Four stratigraphically successive conodont assemblage zones have been recognized in the Lower Carboniferous Codroy Group of southwestern Newfoundland.
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Some isotope age determinations would, at first glance, appear to necessitate radically new concepts of stratigraphic successions and correlations.
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Comparable units to the Génis Unit with an identical stratigraphic succession can be found in the Vendée and in the Rouergue.
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The sequence of the March Formation delineated by these sections yields nearly a complete stratigraphic succession for this formation in southeastern Ontario.
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Four different stratigraphic successions are characteristic of Lower to Middle Devonian, Carboniferous and Permian rocks in the Stikine and Iskut rivers area.
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In the Humber Arm area of the western Newfoundland Appalachians, four distinct stratigraphic successions derived from the Laurentian continental margin are exposed.
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The unpredictable stratigraphical succession is complicated by the prevalence of soft and thinly bedded strata which are hardly detected during soil exploration.
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The ages of the collections are critical to dating the stratigraphic succession of the Lower Paleozoic rocks within the highly deformed terrane.
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A normal–reverse–normal sequence of remanent magnetization was determined within the stratigraphic succession and assigned to the Gauss–Matuyama–Brunhes chrons, respectively.
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The name Leopold Formation is proposed for a thick and distinctive Upper Silurian stratigraphic succession, approximately 1000 ft (305 m) thick, on northeastern Somerset Island.
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Williams' interpretation of the stratigraphic succession and geological history of the cave and its contained deposits, the cultural sequence is described and an explanatory model presented.
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Locally up to 2 km of the stratigraphic succession has been removed, with faults cutting downsection in a westerly direction producing rollover in the hanging wall.
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Till and or ice-contact deposits, glaciomarine sediments, postglacial basinal muds, and bank-top lagoonal sediments grading to sands and gravels make up the stratigraphic succession.
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They correspond to the beginning of sedimentation from more distant sources within the regional Carboniferous stratigraphic succession, which was until then characterized by sedimentation from proximal sources.
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Independently, in 1811, Cuvier and Alexandre Brongniart published an influential study of the geologic history of the region around Paris, based on the stratigraphic succession of rock layers.
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Based on the presence of distinct laterally continuous marker units and similar lithologic ordering, we propose that the Valhalla assemblage is correlative with part of the Palaeozoic North American stratigraphic succession.
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The Antimonio Formation furnishes a record of sedimentation across the Triassic–Jurassic system boundary and is one of a few stratigraphic sections globally that preserves latest Triassic to Hettangian ammonoids in stratigraphic succession.
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From the stratigraphic point of view the cracks are important as they act as traps for fossils and as these fossil-rich fillings are deposited in older rocks, breaking the law of stratigraphic succession.
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The Génis Unit shows the following stratigraphic succession (from top to bottom): Génis greenschist Génis sericite schist Puy-de-Cornut arkose Génis porphyroid The Génis greenschist is the youngest formation of the Génis Unit.
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Recent findings about the late-Precambrian stratigraphic succession in the areas between the Orange River and the Klinghardt Mountains and south of Windhoek throw new light on the relationship between the Damara and Nama Systems.
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A similar stratigraphic succession and tectono-sedimentary history occurring 10–15 Ma earlier at the St. Lawrence Promontory than in the Quebec Reentrant argues for a primary tectonic control for the demise of carbonate sedimentation at the margin.
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82 sinne gevind in 11 ms. Hulle kom uit baie bronne en word nie nagegaan nie.