Search results for "END"

showing 10 items of 32899 documents

Neocomian to early Aptian syn-rift evolution of the normal to oblique-rifted North Gabon Margin (Interior and N'Komi Basins).

2009

18 pages; International audience; The North Gabon coastal rift basins consist of a set of 130–150 long-segment asymmetrically tilted half grabens (Interior Basin) and 000–020 short-segment en échelon half grabens (N'Komi Basin) separated by 040–060 major transverse faults. Tectono-sedimentary analysis of field and subsurface data reveals the control exerted by extensional tectonism over continental sedimentation. During Berriasian to early Barremian times, uniform uniaxial 040–060 extension was responsible for the stretching of the brittle upper crust over a 100-km wide domain. During late Barremian–early Aptian times, the main locus of extension stepped westward resulting in severe end-rif…

010504 meteorology & atmospheric sciencesAptianStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesEarly CretaceousEnd-rift erosionStructural basin010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyEchelon formationGabon0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsRift segmentationRiftOblique riftingGeologyCrust[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCretaceousGrabenTectonics[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyEconomic GeologyPrecambrian heritageNormal riftingGeology
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Spectral biases in tree-ring climate proxies

2013

Seamless quantification of past and present climate variability is needed to understand the Earth’s climate well enough to make accurate predictions for the future. This study addresses whether tree-ring-dominated proxy data properly represent the frequency spectrum of true climate variability. The results challenge the validity of detection and attribution investigations based on these data. External forcing and internal dynamics result in climate system variability ranging from sub-daily weather to multi-centennial trends and beyond1,2. State-of-the-art palaeoclimatic methods routinely use hydroclimatic proxies to reconstruct temperature (for example, refs 3, 4), possibly blurring differe…

010504 meteorology & atmospheric sciencesClimate systemForcing (mathematics)Environmental Science (miscellaneous)010502 geochemistry & geophysics01 natural sciencesFrequency spectrumProxy (climate)13. Climate actionGeneral Circulation ModelClimatologyDendrochronologyEnvironmental sciencePrecipitationSocial Sciences (miscellaneous)0105 earth and related environmental sciencesNature Climate Change
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Temperature Covariance in Tree Ring Reconstructions and Model Simulations Over the Past Millennium

2017

Spatial covariance in the simulated temperature evolution over the past millennium has been reported to exceed that of multiproxy-based reconstructions. Here we use tree ring-based temperature reco ...

010504 meteorology & atmospheric sciencesCovariance functionDendroclimatologyRadiative forcingCovariance010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGeophysicsClimatologyPaleoclimatologyDendrochronologyGeneral Earth and Planetary SciencesSpatial variabilityGeology0105 earth and related environmental sciencesGeophysical Research Letters
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Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?

2012

International audience; Ocean acidification in modern oceans is linked to rapid increase in atmospheric CO 2 , raising concern about marine diversity, food security and ecosystem services. Proxy evidence for acidification during past crises may help predict future change, but three issues limit confidence of comparisons between modern and ancient ocean acidification, illustrated from the end-Permian extinction, 252 million years ago: (1) problems with evidence for ocean acidification preserved in sedimentary rocks, where proposed marine dissolution surfaces may be subaerial. Sedimentary evidence that the extinction was partly due to ocean acidification is therefore inconclusive; (2) Fossils…

010504 meteorology & atmospheric sciencesEffects of global warming on oceansocean acidification010502 geochemistry & geophysics01 natural sciencesEcosystem services14. Life underwaterPermian–Triassic extinction event0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyHigh rateend-Permian extinctionocean acidification; end-Permian extinction; microbialite; ocean buffer; stylolitestylolitelcsh:QE1-996.5fungiBiotaOcean acidificationlcsh:GeologyOceanographymicrobialite13. Climate actionSubaerialGeneral Earth and Planetary SciencesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontologyocean bufferGeologygeographic locations
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Is agro-tourism eco-friendly?

2017

The paper will highlight the impact of agro-tourism on environment in Romania, focusing on the Sibiu County. Thanks to the results obtained from this analysis, research and information collection, the paper will give some answers regarding the question: are agro-tourisms environmentally friendly? The authors identify potential causes of environmental pollution from agro-tourism and some resources that could be economically used. The negative and positive aspects on the increase of agro-tourism activities in the proposed region will be also discussed taking into account there impact on the environment. Based on the obtained results, the authors will propose a method for the management of res…

010504 meteorology & atmospheric sciencesEnvironmental pollution010501 environmental sciencesEnvironmental economics01 natural sciencesEnvironmentally friendlyOrder (business)lcsh:TA1-2040agro-Tourism; environment; pollution;pollutionlcsh:Engineering (General). Civil engineering (General)agro-TourismenvironmentTourism0105 earth and related environmental sciencesMATEC Web of Conferences
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High-grade metamorphism and partial melting of basic and intermediate rocks

2016

Rocks of basic and intermediate bulk composition occur in orogenic terranes from all geological time periods and are thought to represent significant petrological components of the middle and lower continental crust. However, the former lack of appropriate thermodynamic models for silicate melt, amphibole and clinopyroxene that can be applied to such lithologies at high temperature has inhibited effective phase equilibrium modelling of their petrological evolution during amphibolite- and granulite facies metamorphism. In this work, we present phase diagrams calculated in the Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–O2 (NCKFMASHTO) compositional system for a range of natural basic and interm…

010504 meteorology & atmospheric sciencesGeochemistryPartial meltingMetamorphismGeologySolidusengineering.material010502 geochemistry & geophysicsGranulite01 natural sciencesLewisian complexDioriteGeochemistry and PetrologyengineeringPetrologyAmphiboleGeology0105 earth and related environmental sciencesHornblendeJournal of Metamorphic Geology
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A search for time-dependent astrophysical neutrino emission with IceCube data from 2012 to 2017

2020

Abstract High-energy neutrinos are unique messengers of the high-energy universe, tracing the processes of cosmic ray acceleration. This paper presents analyses focusing on time-dependent neutrino point-source searches. A scan of the whole sky, making no prior assumption about source candidates, is performed, looking for a space and time clustering of high-energy neutrinos in data collected by the IceCube Neutrino Observatory between 2012 and 2017. No statistically significant evidence for a time-dependent neutrino signal is found with this search during this period, as all results are consistent with the background expectation. Within this study period, the blazar 3C 279, showed strong var…

010504 meteorology & atmospheric sciencesHigh-energy astronomyAstrophysics::High Energy Astrophysical Phenomenamedia_common.quotation_subjectmodel [emission]FOS: Physical sciencesCosmic rayAstrophysics01 natural scienceslaw.inventionIceCube Neutrino ObservatoryIceCubeblazarlawemission [gamma ray]0103 physical sciencesCosmic ray sources; High-energy astrophysics; Particle astrophysicsenergy: high [neutrino]Blazar010303 astronomy & astrophysics0105 earth and related environmental sciencesmedia_commonHigh Energy Astrophysical Phenomena (astro-ph.HE)astro-ph.HEAstroparticle physicsPhysicsbackgroundAstronomy and AstrophysicsCosmic ray sourcesUniverseHigh-energy astrophysicsmessengerobservatorySpace and Planetary Scienceddc:520time dependenceacceleration [cosmic radiation]NeutrinoAstrophysics - High Energy Astrophysical PhenomenaParticle astrophysicsFlare
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Applications of a new set of methane line parameters to the modeling of Titan's spectrum in the 1.58 μm window

2012

International audience; In this paper we apply a recently released set of methane line parameters (Wang et al., 2011) to the modeling of Titan spectra in the 1.58 mu m window at both low and high spectral resolution. We first compare the methane absorption based on this new set of methane data to that calculated from the methane absorption coefficients derived in situ from DISR/Huygens (Tomasko et al., 2008a; Karkoschka and Tomasko, 2010) and from the band models of Irwin et al. (2006) and Karkoschka and Tomasko (2010). The Irwin et al. (2006) band model clearly underestimates the absorption in the window at temperature-pressure conditions representative of Titan's troposphere, while the Ka…

010504 meteorology & atmospheric sciencesInfraredCASSINI VIMSHUYGENS PROBEMONODEUTERATED METHANEAtmospheric sciences01 natural sciences7. Clean energyMethaneSpectral lineTropospherechemistry.chemical_compoundsymbols.namesake0103 physical sciencesSpectral resolutionSpectroscopy010303 astronomy & astrophysicsCLOUD STRUCTURE0105 earth and related environmental sciencesPhysics[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][PHYS.PHYS.PHYS-OPTICS]Physics [physics]/Physics [physics]/Optics [physics.optics][ PHYS.PHYS.PHYS-OPTICS ] Physics [physics]/Physics [physics]/Optics [physics.optics]Astronomy and Astrophysics9500 CM(-1)SPECTROSCOPIC DATABASEM TRANSPARENCY WINDOWComputational physicsAerosolchemistry[ PHYS.PHYS.PHYS-AO-PH ] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]TEMPERATURE-DEPENDENCE13. Climate actionSpace and Planetary SciencesymbolsSHIFT COEFFICIENTSOUTER SOLAR-SYSTEMTitan (rocket family)
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Shallow system rejuvenation and magma discharge trends at Piton de la Fournaise volcano (La Réunion Island)

2017

International audience; Basaltic magma chambers are often characterized by emptying and refilling cycles that influence their evolution in space and time, and the associated eruptive activity. During April 2007, the largest historical eruption of Piton de la Fournaise (Île de La Réunion, France) drained the shallow plumbing system (>240×106 m3>240×106 m3) and resulted in collapse of the 1-km-wide summit crater. Following these major events, Piton de la Fournaise entered a seven-year long period of near-continuous deflation interrupted, in June 2014, by a new phase of significant inflation. By integrating multiple datasets (lava discharge rates, deformation, seismicity, gas flux, gas composi…

010504 meteorology & atmospheric sciencesLavaeffusive paroxysmMagma chamber010502 geochemistry & geophysicseffusive trend01 natural sciencesEffusive eruptionImpact crater[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryeffusive paroxysm; effusive trends; Piton de la Fournaise; shallow plumbing system; unloading; Geophysics; Geochemistry and Petrology; Earth and Planetary Sciences (miscellaneous); Space and Planetary ScienceGeochemistry and Petrologyunloading[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyEarth and Planetary Sciences (miscellaneous)Petrology0105 earth and related environmental sciencesBasaltgeographygeography.geographical_feature_categoryeffusive trendsFumarolePiton de la FournaiseGeophysicsVolcanoshallow plumbing systemSpace and Planetary ScienceMagmaGeologySeismology
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High-grade metamorphism and partial melting in Archean composite grey gneiss complexes

2016

Much of the exposed Archaean crust is composed of composite gneiss which includes a large proportion of intermediate to tonalitic material. These gneiss terrains were typically metamorphosed to amphibolite to granulite facies conditions, with evidence for substantial partial melting at higher grade. Recently published activity–composition (a-x) models for partial melting of metabasic to intermediate compositions allows calculation of the stable metamorphic minerals, melt production and melt composition in such rocks for the first time. Calculated P–T pseudosections are presented for six bulk rock compositions taken from the literature, comprising two metabasic compositions, two intermediate…

010504 meteorology & atmospheric sciencesMetamorphic rockPartial meltingGeochemistryMetamorphismGeologySolidusengineering.material010502 geochemistry & geophysicsGranulite01 natural sciencesGeochemistry and PetrologyengineeringPetrologyMetamorphic faciesGeology0105 earth and related environmental sciencesGneissHornblendeJournal of Metamorphic Geology
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