Search results for " ROC"

showing 10 items of 951 documents

Apatite and clinopyroxene as tracers for metasomatic processes in nepheline clinopyroxenites of Uralian-Alaskan-type complexes in the Ural Mountains,…

2013

Clinopyroxene and apatite are found to trace metasomatic processes in nepheline-bearing clinopyroxenites (tilaites) from the igneous, mafic-ultramafic Uralian-Alaskan-type complexes of Kytlym and Nizhny Tagil, Ural Mountains, Russian Federation. The clinopyroxenites consist predominantly of coarse-grained, partially to totally altered clinopyroxene phenocrysts in a matrix of fine-grained olivine, clinopyroxene, plagioclase, K-feldspar, and nepheline. Apatite occurs as idiomorphic inclusions (2O-, Na2O-, and Al2O3-bearing fluid. During conversion of the plagioclase, CaO and SiO2 were partitioned into the fluid. Altered areas in the clinopyroxene phenocrysts are characterized by the redistrib…

Fluor-chlorapatiteOlivineCoupled dissolution-reprecipitationFluorapatiteGeochemistryengineering.materialApatiteIgneous rockchemistry.chemical_compoundUralian-Alaskan-type complexeschemistryGeochemistry and PetrologyMetasomatismvisual_artNephelinevisual_art.visual_art_mediumengineeringClinopyroxenePhenocrystPlagioclaseMetasomatismGeology
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Formation processes at a high resolution Middle Paleolithic site: Cueva Antón (Murcia, Spain)

2013

Cueva Anton is a Middle Paleolithic rockshelter located in the valley of the River Mula (Murcia, Spain). The archeological investigation of the site, which began with salvage work in 1991, resumed in 2006 and is still ongoing, uncovered a succession spanning most of MIS 3 and MIS 4 (ca. 75–36 ka) and featuring a well preserved human occupation record. This paper presents the first information about site stratigraphy and site formation processes. Geoarcheological data collected in the field and through micromorphological observation show that the archeological succession at Cueva Anton is mainly composed of alluvial sediments, with thin intercalations of gravitational and slope material. The…

FluvialExcavationEcological successionArchaeologyPrehistòriaPaleontologyStratigraphyMiddle PaleolithicFaciesSedimentary rockAlluviumGeologyEarth-Surface Processes
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Permian-Cenozoic deep-water carbonate rocks of the Southern Tethyan Domain. The case of Central Sicily

2016

We present an integrated stratigraphy of the outcropping and buried Permian-Cenozoic deep-water carbonate successions, forming some of the tectonic units mostly buried beneath the Late Neogene sedimentary cover in the fold and thrust belt of Central Sicily. Three main successions, pertaining to the well known Lercara, Imerese and Sicanian domains, have been reconstructed on the basis of a detailed facies analysis, seismostratigraphic interpretation, bio -stratigraphy (mostly based on palynological data) and comparison between outcropping and subsurface deep-water sediments. The main results reveal a continuous sedimentation of the deep-water Southern Tethyan Sicilian succession since the Pe…

Flysch010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaTerrigenous sedimentCarbonate platformPermian-Cenozoic stratigraphy deep-water carbonates surface and well-log data seismic calibration Central SicilyGeology010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundPaleontologychemistryFaciesGeneral Earth and Planetary SciencesCarbonate rockCarbonateSedimentary rockForeland basinGeology0105 earth and related environmental sciences
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Tetrapod footprint ichno-associations from French Permian basins. Comparisons with other Euramerican ichnofaunas.

2006

21 pages; In order to take into account the studies of the European and American (USA) collections carried out by one of the authors, and of the recent nomenclatural revisions from new footprint discoveries, which have occurred during the last decade, the authors present a critical review of the French Permian palichnofauna. The distribution of the ichnospecies in the stratigraphy of the Lodève Basin, taken as a reference, is outlined. The ichno-associations are then compared with those of other French (Provence), European (Italy, Germany) and USA basins. Based on the ages of different ichnofossiliferous formations, three successive ichnofaunal units can be distinguished in the Permian of E…

FootprintPaleontologyStratigraphyPermianTetrapod (structure)GeologyOcean EngineeringSedimentary rock[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyStructural basinGeologyWater Science and Technology[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Sedimentary features reveal transport paths for Holocene sediments on the Kristianstad coastal plain, SE Sweden.

2017

AbstractWe have investigated coastal and aeolian deposits on the Kristianstad plain in southernmost Sweden by a combination of methods that has yielded data on sedimentary features such as grain-size variations, shape and character of quartz grain surfaces (determined in light microscope and scanning electron microscope), and mineralogical composition. Such sedimentary techniques have been not applied to coastal deposits in this part of the Baltic Sea region before. The littoral, foredune and parabolic dune sands are sedimentologically similar, only a slight grain-size transformation by aeolian processes in the foredune was observed. Sand in straight-crested dunes, on the other hand, origin…

Foredunegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesCoastal plainMaturity (sedimentology)GeochemistryPaleontologyGeology010502 geochemistry & geophysics01 natural sciencesPaleosolLittoral zoneAeolian processesSedimentary rockQuartzGeomorphologyGeology0105 earth and related environmental sciences
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Testing a portable laser-induced breakdown spectroscopy system on geological samples.

2012

9 pages; International audience; This paper illustrates the potentialities of a home-made portable LIBS (laser-induced breakdown spectroscopy) instrument in Earth sciences, more particularly in geochemically recognizing (i) tephra layers in lacustrine sediments and (ii) fossilization processes in ammonites. Abundances for selected lines of Al, Ca, Fe, Ti, Ba and Na were determined in lacustrine chalk sediments of the Jura, where the Laacher See Tephra (LST) layer is recorded. A statistical treatment of elemental maps produced from the section of a sedimentary column containing the LST event allows instrumental conditions to be optimized. Accumulating spectra from close shot positions gives …

Fossilization[SDE.MCG]Environmental Sciences/Global ChangesMineralogy02 engineering and technology[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSpectral lineAnalytical Chemistry[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLIBS cartographyAmmoniteLaser-induced breakdown spectroscopySpectroscopyTephraInstrumentationSpectroscopy[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonite010401 analytical chemistry021001 nanoscience & nanotechnology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAtomic and Molecular Physics and Opticslanguage.human_language0104 chemical sciences[ SDE.MCG ] Environmental Sciences/Global ChangesPortable LIBSTephra[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageSedimentary rock0210 nano-technology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Source composition, fractional crystallization and magma mixing processes in the 3.48–3.43Ga Tsawela tonalite suite (Ancient Gneiss Complex, Swazilan…

2016

Abstract The ca. 3480–3430 Ma Tsawela Gneiss (TG) is a well-preserved coarse-grained diorite to tonalite suite within the Ancient Gneiss Complex of Swaziland, eastern Kaapvaal craton. These gneisses are texturally and compositionally distinct from the hosting oldest components of the ca. 3200–3660 Ma TTG-type Ngwane Gneisses (NG). Major and trace elements, in combination with whole-rock hafnium-neodymium isotopic data, were analyzed in the TG and in three samples of ca. 3450 Ma grey NG to constrain sources and magmatic processes. High-field-strength element data (HFSE) were combined with U-Pb SHRIMP II ages and Hf-in-zircon data for key samples to constrain their ages and petrogenesis. In c…

Fractional crystallization (geology)010504 meteorology & atmospheric sciencesContinental crustGeochemistryGeologyCrust010502 geochemistry & geophysics01 natural sciencesDioriteIgneous rockGeochemistry and PetrologyIgneous differentiationMaficGeology0105 earth and related environmental sciencesGneissPrecambrian Research
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Torngat ultramafic lamprophyres and their relation to the North Atlantic Alkaline Province

2004

Geological mapping and diamond exploration in northern Quebec and Labrador has revealed an undeformed ultramafic dyke swarm in the northern Torngat Mountains. The dyke rocks are dominated by an olivine-phlogopite mineralogy and contain varying amounts of primary carbonate. Their mineralogy, mineral compositional trends and the presence of typomorphic minerals (e.g. kimzeyitic garnet), indicate that these dykes comprise an ultramafic lamprophyre suite grading into carbonatite. Recognized rock varieties are aillikite, mela-aillikite and subordinate carbonatite. Carbonatite and aillikite have in common high carbonate content and a lack of clinopyroxene. In contrast, mela-aillikites are richer …

Fractional crystallization (geology)OlivineProterozoicGeochemistryGeologyengineering.materialGeochemistry and PetrologyUltramafic rockCarbonatiteengineeringLaurentiaMaficPetrologyAmphiboleGeologyLithos
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El pintor Carreño y el retablo del Convento de Predicadores de Valencia

2010

Francisco A. 67 81UNESCO::CIENCIAS DE LAS ARTES Y LAS LETRAS:CIENCIAS DE LAS ARTES Y LAS LETRAS [UNESCO]0211-5808 9678 Archivo de arte valenciano 277874 2010 91 3629742 El pintor Carreño y el retablo del Convento de Predicadores de Valencia Roca Traver
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The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths

2021

We present the first isotopic (noble gases and CO2) characterization of fluid inclusions coupled to Raman microspectroscopy analyses in mantle xenoliths from Central Mexico, a geodynamically complex area where the Basin and Range extension was superimposed on the Farallon subduction (terminated at 28 Ma). To characterize the isotopic signature of the Central Mexican lithospheric mantle, we focus on fluid inclusions entrapped in mantle xenoliths found in deposits of the Joya Honda maar (JH), a Quaternary monogenetic volcano belonging to the Ventura Espiritu Santo Volcanic Field (VESVF) in the state of San Luis Potosí (central Mexico). Thirteen ultramafic plagioclase-free xenoliths were selec…

GEO/07 - PETROLOGIA E PETROGRAFIA010504 meteorology & atmospheric sciencesCarbonate recyclingGeochemistry2010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundNoble gaseGeochemistry and PetrologyUltramafic rockGEO/08 - GEOCHIMICA E VULCANOLOGIAXenolithFluid inclusionsMetasomatismFarallon Plate0105 earth and related environmental sciencesMantle refertilizationSubductionGeologyFluid inclusionSilicateCOchemistryCarbonate recycling CO2 Fluid inclusions Mantle refertilization Mexican mantle xenoliths Noble gasesGeologyMexican mantle xenolith
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