Search results for "CARBONATE PLATFORM"

showing 10 items of 87 documents

Sedimentology, petrography and geochemistry of a limestone breccia (Pietra di Billiemi) from NW Sicily, Italy: implications for evolution of the Teth…

2009

In this study, the Pietra di Billiemi, a famous dimension stone, is investigated because it records the tectonic evolution of the south Tethys continental margin and preserves a record of major environmental changes occurring near the Triassic/Jurassic boundary. The Pietra di Billiemi is a grey, coarse-grained and clast-supported limestone breccia cropping out in an area of the Palermo Mountains representing a segment of the Apennine–Maghrebian chain in western Sicily. The rock consists of metre-sized to centimetre-sized angular clasts, derived from Upper Triassic sponge boundstones and rudstones, with a differently coloured, silt-grained matrix. Fitted fragments are observed commonly which…

MicriteCarbonate platformStratigraphyAnoxic conditions authigenic minerals in situ breccia isotopes Sicily Triassic–Jurassic boundary.DolomiteGeochemistryGeologyAuthigenicPetrographyPaleontologychemistry.chemical_compoundchemistryAnoxic conditions; Authigenic minerals; In situ breccia; Isotopes; Sicily; Triassic-Jurassic boundary; Geology; StratigraphyBrecciaCarbonateSedimentologyGeology
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LES VARIATIONS DU NIVEAU MARIN SUR LE BASSIN DE PARIS AU BATHONIEN-CALLOVIEN. IMPACTS SUR LES COMMUNAUTÉS BENTHIQUES ET SUR L'ÉVOLUTION DES ORNITHELL…

1992

The study deals with the biological impacts of sea-Ievel changes on evolution of a Jurassic benthic fossil group (Ornithellida, Brachiopoda). The different time and scale at which the shifts in marine environments occur leads to the recognition of three interacting dynamic systems: environmental, communities, populations dynamics. The analysis is thus divided into a three steps hierarchy: sequence stratigraphy, analysis of the diversity of brachiopod assemblages, and analysis of morphological variations within omithellid populations. Sequence stratigraphy of the Dogger marly and carbonate successions in the Paris basin provides accurate correlations of depositional environments from shallow…

Ornithellidssequence stratigraphyJurassique moyenbrachiopodes[SDU.STU]Sciences of the Universe [physics]/Earth SciencescyclesdiversityMiddle Jurassiccarbonate platformmorphologydiversitérétroaction taphonomiqueOrnithellidéscontraintes écologiques et historiquestaphonomic feedbackbiostratigraphie[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesParis basinStratigraphie séquentielleplateforme carbonatéemorphologie[SDU.STU] Sciences of the Universe [physics]/Earth Sciencesecologieal and historical constraintsbassin de Parisbiostratigraphybrachiopods
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Ladinian carbonates of the Cabo Cope Unit (Betic Cordillera, SE Spain): a tethys-maláguide palaeogeographic gateway.

2003

7 pages, 4 figures.

OutcropCarbonate platformDaonellaStratigraphyMaláguide ComplexSephardiellaPaleontologychemistry.chemical_compoundDaonellaPosidoniaSedimentologyTethysbiologyTriassic (Ladinian)PaleontologyGeologyLadinianbiology.organism_classificationBetic BasinchemistrySpainClastic rockAlpine Faunal ProvinceCarbonate PlatformCarbonate rockCarbonatePalaeogeographyGeologySephardic Faunal Province
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Oxfordian paleobiogeographic perturbation between the Iberian and Sicilian regions: the role of the Panormide Carbonate Platform.

2006

Oxfordian paleobiogeographic Iberia Sicily Panormide Carbonate Platform
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Carbonate Platform-Basin Transition in SW Sicily. Implications for the paleogeographic reconstruction of the Central Mediterranean area.

2010

PALEOGEOGRAPHY SICILY CARBONATE PLATFORM BASIN
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Stratigraphic and structural relationships between Meso-Cenozoic Lagonegro basin and coeval carbonate platforms in southern Apennines, Italy

1999

Abstract Stratigraphic studies and facies analysis integrated with a new geological and structural survey of the Meso-Cenozoic units outcropping in the Campania–Lucania Apennines, southern Italy, allowed us to restore the palaeogeographic pattern and the tectonic evolution of the chain during Oligo-Miocene times. The southern Apennines are a N150°-striking and NE-verging fold-and-thrust belt mainly derived from the deformation of the African–Apulian passive margin. Four wide belts with different features have been recognized in the chain area. From east to west the following units outcrop: (a) successions characterized by basinal to marginal facies, ranging in age from Cretaceous to Miocene…

PaleontologyGeophysicsPassive marginCarbonate platformOutcropFaciesSiliciclasticNeogeneCenozoicGeologyCretaceousEarth-Surface ProcessesTectonophysics
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The Panormide Carbonate Platform (Sicily): an anomalous case in the evolution of Jurassic Tethyan basins.

2007

Panormide Carbonate Platform Sicily Tethyan
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The structure of western Sicily, central Mediterranean

2002

Western Sicily is part of the Sicilian chain, a sector of the SE-verging Alpine orogenic belt in the central Mediterranean. Interpretation of seismic reflection profiles, boreholes and recent inland geological data, have enabled us to assess the deep structural grain. A wedge of flat-lying Mesozoic–Miocene carbonate and terrigenous rocks (pre-Panormide nappes) is superimposed on NW-trending, 7–8 km thick, Mesozoic–Paleogene carbonate thrust ramps (Trapanese units), arranged in two structural levels extending from the Tyrrhenian coast to western offshore Sicily. Upper Miocene to Pleistocene terrigenous strata, often deformed, fill syntectonic basins above the thrust pile. The main tectonic t…

PleistoceneTerrigenous sedimentCarbonate platformGeologyLate MioceneTranspressionNappeAllochthonPaleontologychemistry.chemical_compoundFuel TechnologychemistryGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)CarbonateEconomic GeologyGeology
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Tectono-biosedimentary recordings at the Lias-Dogger transition: example of the Quercy carbonate platform (Aquitaine Basin, France).

2007

AbstractOn the eastern edge of the Aquitaine Basin, the Lias-Dogger transition and the events, which occurred during this time interval are studied in the Quercy sedimentary basin. Stratigraphic correlations are proposed using a biochronological calibration based on the determination of numerous ammonites and brachiopods. Facies analyses using statistical processing integrate the presence of faults and tectonic compartments and lead to reconstruction of palaeoenvironments in space and time. The paper includes the description of system tracts following Haq et al. [1987] and Vail et al. [1991], and twelve palaeogeographic maps of the area studied. The objectives are to distinguish the various…

QuercyAalenian010504 meteorology & atmospheric sciencesCarbonate platform[SDE.MCG]Environmental Sciences/Global Changes[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/TectonicsToarcianStructural basin010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStatistical processing0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryTectonicsGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsSedimentary basinTectonics[ SDE.MCG ] Environmental Sciences/Global ChangesCarbonate platform[SDE.MCG] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFacies[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyFranceSedimentationGeology
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Detrital zircon and micropalaeontological ages as new constraints for the lowermost tectonic unit (Talea Ori unit) of Crete, Greece

2007

The Talea Ori unit is the lowermost known tectonic unit of Crete and the most external part of the Hellenides. Its stratigraphy ranges from Late Carboniferous to Oligocene and outcrops of the lower part are only known in the Talea Ori mountains (central Crete). In this area, a black sandstone at the base of the Galinos Beds, thought to be the oldest formation, contains zircons which were dated using the single grain evaporation method. The majority of these grains yielded Late Carboniferous ages (Variscan), while a small group yielded Early Proterozoic ages. The age distribution of these zircons suggests that, at the Carboniferous–Permian boundary, not much of the older North Gondwanan base…

RiftPermianProterozoicCarbonate platformEarly TriassicPaleontologyDetrital zirconForaminiferaPermianOceanographyCreteTriassicConglomeratePaleontologyBasement (geology)Carboniferousddc:550External HellenidesEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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