stratigraphic sequence of rocks oor Frans
stratigraphic sequence of rocks
Vertalings in die woordeboek Engels - Frans
succession lithostratigraphique
séquence lithostratigraphique
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
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The supracrustal rocks occur in well-defined stratigraphic sequences of varied metasediments, gneisses, and charnockites.
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South of the LLSD, large-scale, northwest-trending folds involve basaltic sequences that are stratigraphically overlain by thick sections of dacitic volcaniclastic and turbiditic rocks.
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Despite being designed during an early and somewhat primitive stage of the science of geology, it is remarkable how accurate these sections were, describing a sequence of 36 stratigraphical levels in Derbyshire rocks with a lengthy fold-out cross-section of almost the entire width of Derbyshire.
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One of the difficulties of assigning ages to rock strata by this means is referred to by Henry Faul, in his book, Ages of Rocks, Planets, and Stars: “Rocks that are suitable for age measurement and at the same time reliably correlated with the stratigraphic sequence are very rare.”
estime que la délégation ne représente pas dans tous les cas une formule optimale, compte tenu des frais supplémentaires afférents aux collaborateurs locaux et de l'impossibilité de déléguer certaines fonctionsjw2019 jw2019
The age and gross lithology of the Chilkat Peninsula sequence are comparable to Upper Triassic rocks that characterize the allochthonous tectono-stratigraphic terrane named Wrangellia.
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The volcanic rocks of the Aspy terrane differ from many other Silurian and Silurian–Devonian successions in Atlantic Canada, which have chemical and stratigraphic characteristics of volcanic rocks formed in extensional within-plate settings, and are somewhat younger than the Aspy terrane sequences.
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The stratigraphic and structural characteristics of the Midway sequence are generally similar to those of the Timiskaming Group and Timiskaming-type rocks in Canada, and more specifically to those of the Shebandowan Group in the Thunder Bay district.
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Some of the volcano-sedimentary strata within this succession, however, contain foliated clasts of Baggs Hill Granite, and these strata must comprise a younger stratigraphic sequence which, in this area, is thrust northwestward over the older rocks.
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In this paper, we present the nature and meaning of the archaeological deposits at Takarkori rock shelter, where a relatively large area has been recently excavated, showing a stratigraphic sequence extending from c. 9,000 to 4,200 BP, unevenly represented by several occupation pulses.
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The juvenile arc tectono-stratigraphic assemblages are generally marked by older and stratigraphically lower tholeiitic submarine volcanic packages (ca. 1.903-1.886 Ga) that are observed or interpreted to be overlain by extensive and lithologically varied sequences of calc-alkaline and alkaline (shoshonitic) arc rocks and arc rift deposits (ca.
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According to the geological map and the regional stratigraphic sequence, the rock substratum should be made of Cretaceous grey limestone.
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Alkaline volcanic rocks, sometimes feldspathoid bearing, appear in variable stratigraphic positions within the Eocene of the middle part of Central Iran. No magmatic zonation and no K2O enrichment in both time and space can be found in this volcanic sequence.
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This rock shelter yielded a stratigraphic sequence of the main Pastoral occupations in the Tadrart Acacus.
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The pole positions for Circum-Superior orogen rocks, the Proterozoic outliers, and the Sutton Lake inlier suggest: (1) a time-stratigraphic correlation between the LG-4 Sakami, Dieter Lake, Sutton Lake, and the upper part of the Belcher Island sequences; and (2) a time-stratigraphic correlation between the lower part of the Belcher Islands sequence and the Richmond Gulf sequence, which must be substantially older than group 1.
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A symmetrical repetition of the footwall–iron formation–hanging wall stratigraphic sequence is observed in DDH-B357, with distinct felsic volcanic rock domains separated by the three iron formations.
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Geo Territorial Museum The GeoTerritorial Museum first proposes a presentation explaining the birth and evolution of the planet Earth, followed by a tour which begins with a clear prologue, the stratigraphic sequence typical of the Umbro-Marchigiana area, which is a prelude to the analysis of the rocks which characterise the territory of Cantiano.
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These occurrences are located in stratigraphy situated south of the Lower Detour Deformation Zone placing them in the same stratigraphic rock sequence which, on a regional basis hosts both the Selbaie and Mattagami VMS camps to the southeast.
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This precise age determination for the classic Paleoproterozoic stratigraphic sequence of northern Michigan, the Marquette Range Supergroup (MRS), necessitates modification of previous depositional and tectonic intruded Middle Proterozoic Purcell Supergroup rocks in southeastern British Columbia.
Le règlement (CE) n° # de la Commission du # avril # autorisant provisoirement lParaCrawl Corpus ParaCrawl Corpus
18 sinne gevind in 17 ms. Hulle kom uit baie bronne en word nie nagegaan nie.