Search results for " carbonati"

showing 10 items of 13 documents

An overview of the geochemical characteristics of oceanic carbonatites: New insights from Fuerteventura carbonatites (Canary islands)

2021

The occurrence of carbonatites in oceanic settings is very rare if compared with their continental counterpart, having been reported only in Cape Verde and Canary Islands. This paper provides an overview of the main geochemical characteristics of oceanic carbonatites, around which many debates still exist regarding their petrogenesis. We present new data on trace elements in minerals and whole-rock, together with the first noble gases isotopic study (He, Ne, Ar) in apatite, calcite, and clinopyroxene from Fuerteventura carbonatites (Canary Islands). Trace elements show a similar trend as Cape Verde carbonatites, almost tracing the same patterns on multi-element and REE abundance diagrams. 3…

CalciteCape Verdelcsh:Mineralogylcsh:QE351-399.2010504 meteorology & atmospheric sciencesCape Verde Fuerteventura Noble gases isotopes Oceanic carbonatites Trace elementsnoble gases isotopesGeochemistrytrace elementsGeology010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesLithospheric mantleMantle (geology)Cape verdeFuerteventurachemistry.chemical_compoundchemistryCarbonatiteoceanic carbonatitesGeology0105 earth and related environmental sciencesPetrogenesis
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Il carsismo nei rilievi carbonatici della Sicilia Nordoccidentale.

2007

Carsismo Sicilia nord-occidentale carbonati
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On the physico-chemical evolution of low-pH and CEM I cement pastes interacting with Callovo-Oxfordian pore water under its in situ CO2 partial press…

2014

International audience; Abstract Within the framework of geological repositories for radioactive waste, structural concretes must be adapted to the underground chemical conditions. CEM I cement-based materials are characterised by high pH that may produce an alkaline plume in the near-field of the repository. In order to avoid this problem, low-pH cements have been designed. This study compares the physico-chemical behaviour of a low-pH material with a CEM I cement paste, both being subjected to leaching by an aqueous solution. An original experimental setup was designed to reproduce the underground conditions using a specific CO2 regulation device. Under these conditions, the low-pH materi…

CementMaterials scienceAqueous solutionta114Precipitation (chemistry)Microstructure (B) Carbonation (C) Cement paste (D) Durability (C) Degradation (C)MineralogyRadioactive wasteBuilding and Construction010501 environmental sciences010502 geochemistry & geophysicsMicrostructure01 natural sciencesPore water pressureChemical engineeringGeneral Materials Science[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]Leaching (metallurgy)Porosity0105 earth and related environmental sciencesCement and Concrete Research
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The geochemistry of the Barra do Itapirapua carbonatite (Ponta Grossa Arch, Brazil): a multiple stockwork

2002

The Early Cretaceous Barra do Itapirapuā carbonatite, in southern Brazil, belongs to the initial stages of the alkaline carbonatitic magmatism in the Ponta Grossa Arch Province, as related to the opening of the south Atlantic Ocean. The magmatic evolution of the complex comprises four phases of intrusive carbonatite that are composed of medium- to coarse-grained Mg and Fe carbonatites with small volumes of late fine- to very fine-grained Mg carbonatites and show evidence of pervasive hydrothermal events. Drill core samples reveal the existence of silicate rocks of syenitic composition of two different origins. Among the silicate rocks, there are syenites of a likely magmatic origin, as well…

FenitizationStockworkFractional crystallization (geology)Fenitization; Carbonatite; SyeniteGeochemistryGeologySilicatechemistry.chemical_compoundchemistryEarth-Surface ProcesseMagmatismCarbonatiteSyeniteCarbonatiteIgneous differentiationProtolithGeologyEarth-Surface ProcessesWall rock
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“Operative propoals for resisting the phenomenon of the seawater intrusion along the coast of the eastern Sicily"

2003

INTRUSIONE SALINAACQUIFERO CARBONATICO
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Carbonatites from the southern Brazilian Platform: A review. II: Isotopic evidences

2020

Early and Late Cretaceous alkaline and alkaline–carbonatitic complexes from southern Brazil are located along the main tectonic lineaments of the South America Platform. Calcium-, magnesium-, and ferrocarbonatites are well represented and frequently associated even in the same complex. Primary carbonates present significant variations in C–O isotopic compositions, which are mainly due to isotope exchange with H2O–CO2-rich hydrothermal fluids, whereas fractional crystallization or liquid immiscibility probably affects the δ18O and δ13C values by no more than 2δ‰. Our isotope exchange model implies that the most significant isotopic variations took place in a hydrothermal environment, e.g., i…

QE1-996.5carbonatites: southern brazilcarbonatites; southern Brazil; C-O isotopes; Sr-Nd-Pb-Re-Os systematicC-O isotopesGeologysouthern Brazilcarbonatitessr–nd–pb–re–os systematicC-O isotopes carbonatites: Southern Brazil Sr-Nd-Pb-Re-Os systematicc–o isotopesSr-Nd-Pb-Re-Os systematic
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La Piattaforma Carbonatica Panormide: un caso anomalo nell'evoluzione dei bacini della Tetide giurassica

2010

Negli ultimi anni sono state proposte diverse ricostruzioni paleogeografiche dell'area Centro Mediterranea durante il Mesozoico.La Piattaforma Carbonatica Panormide (PCPA) viene collocata tra la Tetide Alpina e la Tetide Ionica, in un'area geodinamicamente molto complessa. Recenti studi hanno documentato la presenza di superfici di discontinuita che caratterizzano l'evoluzione stratigrafica della PCPA rispetto alle adiacenti Piattaforme Carbonatiche Siciliane. La presenza di superfici di discontinuita negli intervalli Retico-Hettangiano e Giurassico Medio-Oxfordiano vengono messe in relazione, attraverso il confronto della storia della subsidenza tra le Piattaforme Carbonatiche, con gli sta…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaGeneral Earth and Planetary SciencesGeologyDiscontinuità paleogeografia Piattaforma Carbonatica Panormide Sicilia subsidenza
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Utilizzazione pratica delle carte di vulnerabilità degli iblei”

2009

Settore GEO/05 - Geologia Applicatavulnerabilità delle falde regime pluviometrico insalinamento sorgenti sottomarine acquiferi carbonatici fratturati e carsificati
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Ca-rich carbonates associated with ultrabasic-ultramafic melts. Carbonatite or limestone xenoliths? A case study from the late Miocene Morron de Vill…

2016

The volcanic products of the late Miocene Morron de Villamayor volcano (Calatrava Volcanic Field, central Spain) are known for being one of the few outcrops of leucitites in the entire circum-Mediterranean area. These rocks are important because aragonite of mantle origin has been reported as inclusion in olivine macrocrysts. We use petrographic observations, mineral compositions, as well as oxygen and carbon isotope ratios coupled with experimental petrology to understand the origin of carbonate phase in these olivine-phyric rocks. Groundmass and macrocryst olivines range from δ18OVSMOW of +4.8‰, typical of mantle olivine values, to +7.4‰, indicating contamination by sedimentary carbonate.…

alkali basalts010504 meteorology & atmospheric sciencesGeochemistrySkarnMediterraneanengineering.material010502 geochemistry & geophysics01 natural sciencespetrologygeochemistry; petrology; carbonate; carbonatite; olivine; mantle; alkaline; Spain; Cenozoic; MagmatismPetrographychemistry.chemical_compoundcarbonateGeochemistry and PetrologyUltramafic rockolivineNeogene volcanism0105 earth and related environmental sciencesgeochemistryPeridotiteOlivineCenozoicAragoniteMagmatismcarbonatitechemistry13. Climate actionSpainCarbonatiteengineeringCarbonatealkalineGeologymantle
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Preliminary results of fault-related permeability structures associated in the Scicli-Ragusa fault, Hyblean Plateau, Sicily.

2010

architettura di faglia carbonati miocenici di piattaforma e rempa permeabilità delle faglieplateau Ibleo.Settore GEO/03 - Geologia Strutturale
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