Search results for "Sedimentary basin"

showing 10 items of 27 documents

Fires at Neumark-Nord 2, Germany: An analysis of fire proxies from a Last Interglacial Middle Palaeolithic basin site

2016

Few sites with evidence for fire use are known from the Last Interglacial in Europe. Hearth features are rarely preserved, probably as a result of post-depositional processes. The small postglacial basins (

010506 paleontologyArcheologyHearthEemianStructural basinHeated flint01 natural sciencesLast InterglacialBurned bone0601 history and archaeologyCharcoalheated flint0105 earth and related environmental sciencesFire usegeographyEemiangeography.geographical_feature_category060102 archaeology06 humanities and the artsSedimentary basinArchaeologysedimentary basinsburned bonevisual_artCharcoalInterglacialvisual_art.visual_art_mediumGeologycharcoal
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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe

2011

AbstractAn interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

010506 paleontologyEemiangeographyPaleomagnetismgeography.geographical_feature_category010504 meteorology & atmospheric sciencesAardwetenschappenBlake EventMIS 5ePalaeomagnetismLast interglacialTime lagLate onsetEemianSedimentary basin01 natural sciencesSequence (geology)PaleontologyArts and Humanities (miscellaneous)InterglacialShort PaperGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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Basin analysis in the Southern Tethyan margin: Facies sequences, stratal pattern and subsidence history highlight extension-to-inversion processes in…

2018

Abstract In the Mediterranean, the South-Tethys paleomargin experienced polyphased tectonic episodes and paleoenvironmental perturbations during Mesozoic time. The Cretaceous shallow-water carbonate successions of the Panormide platform, outcropping in the northern edge of the Palermo Mountains (NW Sicily), were studied by integrating facies and stratal pattern with backstripping analysis to recognize the tectonics vs. carbonate sedimentation interaction. The features of the Requienid limestone, including geometric configuration, facies sequence, lithological changes and significance of the top-unconformity, highlight that at the end of the Lower Cretaceous the carbonate platform was tecton…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW SicilyCarbonate platformVertical movementStratigraphyInversion (geology)Geology010502 geochemistry & geophysicsCretaceou01 natural sciencesCretaceousCarbonate platformchemistry.chemical_compoundPaleontologyTectonicschemistryFaciesSedimentary basin analysisCarbonateExtensional tectonicsPositive tectonic inversionGeology0105 earth and related environmental sciencesSedimentary Geology
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Carbon and Oxygen Isotope Signals from the Callovian–Oxfordian in French Sedimentary Basins

2013

3 pages; International audience; High-resolution carbon and oxygen isotope data from the Paris Basin and the Subalpine Basin (France) are available in a precise biostratigraphic framework for the Callovian-Oxfordian stages. A biostratigraphically well-constrained δ13C curve, derived from bulk carbonates in the Paris Basin and the Subalpine Basin, is provided in order to document carbon-cycle evolution and to serve as a chemostratigraphic reference for the Callovian-Oxfordian in the Tethyan domain. Sea-temperature reconstructions, using diagenetically screened belemnite and oyster data, reveal major climate perturbations at the Middle-Late Jurassic transition.

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesCallovianBelemnitechemistry.chemical_elementStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CBivalveCarbon cycleSedimentary basin[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPalaeotemperatures[ SDE.MCG ] Environmental Sciences/Global Changeschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMontane ecologyCarbonGeology
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The origin and timing of multiphase cementation in carbonates: Impact of regional scale geodynamic events on the Middle Jurassic Limestones diagenesi…

2009

The Middle Jurassic carbonates of the eastern part of the Paris Basin display surprisingly low values of porosity and permeability (Φ < 15‰ and K < 0.5 mD). The main objective of this study is to determine the causes and timing of the cementation that altered the petrophysical properties of these carbonates thereby destroying their potential as oil reservoirs; a fate that did not befall their equivalents in deeper, central parts of the Paris Basin. Using petrographic and geochemical analyses (stable O and C isotopes, Sr isotopes, major elements), we identify six calcitic spar stages, two dolomite stages, and several episodes of fracturing and stylolitization ordered in paragenetic sequence.…

Calcitegeographygeography.geographical_feature_categoryStratigraphyDolomiteGeochemistryGeologySedimentary basinCementation (geology)UnconformityCretaceousDiagenesischemistry.chemical_compoundPaleontologychemistryMeteoric waterGeologySedimentary Geology
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Structural highs formation and their relationship to sedimentary basins in the north Sicily continental margin (southern Tyrrhenian Sea): implication…

2005

Two high-penetration seismic profiles across the continental margin of north Sicily (southern Tyrrhenian Sea) have been interpreted to construct a crustal section across the margin and to provide a three-dimensional perspective on the upper crustal setting of the Solunto High and its structural relationships with the adjacent Cefalù Basin. Crystalline rocks of the Kabilian-Calabrian Units (KCU) are recognized in the Solunto High region and farther to the north. The KCU body is tectonically superimposed onto sedimentary rocks pertaining to the Sicilian-Maghrebian Units (SMU) and the Solunto High corresponds to the thrust sheet culmination. Its occurrence in the Solunto High demonstrates that…

Continental collisionBACK-ARC BASINSUBSIDENCELate MioceneNappe/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterPaleontologyContinental marginSDG 14 - Life Below WaterKINEMATICSGeomorphologyEarth-Surface Processesgeographygeography.geographical_feature_categorySubductionAPENNINESCONSTRAINTSSedimentary basinEVOLUTIONLITHOSPHEREINSIGHTSGeophysicsBack-arc basinSedimentary rockGeologyHIGH-RESOLUTIONEXTENSION
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Sedimentology and sequence stratigraphy of wedge-top clastic successions: Insights and open questions from the upper Tortonian Terravecchia Formation…

2013

Abstract An up to 1250 m-thick clastic succession, the upper Tortonian Terravecchia Formation (TRV), has been analysed in detail in the middle–late Miocene Scillato wedge-top Basin grown above an already deformed tectonic stack in the northern Sicilian fold-and-thrust belt. The study involved field-based sedimentological and stratigraphic analyses aimed to determine to what extent both the depositional and sequence stratigraphic evolution of the Scillato Basin have been ruled by syn-sedimentary compressional to transpressional tectonics. Widespread intraformational angular unconformities associated with sudden change of palaeocurrents pattern and successive source area shifting suggest that…

DeltaSyntectonic basinSequence stratigraphySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyGeologyOceanographyUnconformitySedimentary depositional environmentPaleontologyGeophysicsClastic rockFaciesSedimentary basin analysisEconomic GeologySequence stratigraphyDepositional sequenceSedimentologyBasin analysiGeologyMarine and Petroleum Geology
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An anomalous case in the evolution of the Mesozoic sedimentary basins between Alpine and Ionian Tethys: the Panormide Carbonate Platform (Sicily).

2007

Mesozoic sedimentary basins Alpine and Ionian Tethys Panormide Carbonate Platform Sicily
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Large- and small-mammal distribution patterns and chronostratigraphic boundaries from the Late Pliocene to the Middle Pleistocene of the Italian peni…

2007

Abstract Over the last 50 years the studies on terrestrial mammals of the Italian peninsula have provided a large volume of data and a more detailed knowledge of faunal events during the Late Pliocene and Quaternary. Moreover geological, sedimentological, palynological and magnetostratigraphical investigations on the Pliocene–Pleistocene continental sedimentary basins have yielded the possibility of a detailed calibration of the faunal successions. Thus, palaeontologists have been able to reconstruct faunal sequences and to propose biochronological scales based on large and small mammals, respectively. In the present contribution an integration of the two biochronological scales is proposed…

Palynologygeographygeography.geographical_feature_categoryPleistocenechronostratigraphical boundariesSmall mammalSedimentary basinIntegrated approachLate Pllioce-Middle PleistoceneLarge and small mammals; distribution patterns; chronostratigraphical boundaries; Late Pllioce-Middle Pleistocene; Italian peninsuladistribution patternsSequence (geology)PaleontologyPeninsulaPleistocene mammals bio-chronology ItalyQuaternaryGeologyLarge and small mammalsItalian peninsulaEarth-Surface Processes
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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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