Search results for "MINERALOGY"

showing 10 items of 1516 documents

An Overview of the Hypogene Caves of Sicily

2017

Karst in Sicily develops in both Messinian gypsum and Mesozoic or Tertiary limestone rocks. Caves are also found in the basalts of Mount Etna. Except for some rare cases, until recently most caves developed in limestone were considered to be of epigenetic origin. The discovery of gypsum in some of these caves, and especially detailed morphological studies, have allowed defining a hypogenic origin for a dozen of caves up to now. In some of these, the hypogenic evidences are very clear, while others remain in doubt because of the widespread presence of well-developed condensation-corrosion morphologies not necessarily related to hydrothermal fluids. This paper reports the present knowledge of…

Basaltgeography.geographical_feature_category010504 meteorology & atmospheric sciencesHypogeneSettore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistryMineralogy010502 geochemistry & geophysicsKarst01 natural sciencesGeographyHypogenic caves Sicily Sulfuric acid speleogenesis Condensation-corrosion Wall sculpturingCaveHypogenic caves Sicily Sulfuric acid speleogenesis Condensation-corrosion Wall sculpturingMesozoic0105 earth and related environmental sciences
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Investigation of the He solubility in H2O-CO2 bearing silicate liquids at moderate pressure: a new experimental method

2000

We have designed the first available experimental method capable to investigate the solubility of inert gases in H2O–CO2 bearing silicate melts in a large range of pressures. The method overcomes the difficulties imposed by the physical state of volatiles at room conditions. Experiments were done by using an internally heated pressure vessel, where sealed capsules containing the sample are introduced. The peculiarity of the method consists in the capability of loading, in accurately known proportions (even lower than ppm), volatiles in a gaseous state at room conditions. Gas is loaded as a weighed amount of a gas-bearing glass, which was previously prepared by using the same gas as a pressu…

BasaltsolubilityMineralogyNoble gaschemistry.chemical_elementheliumSilicatePressure vesselMantle (geology)chemistry.chemical_compoundpressureGeophysicschemistryChemical engineeringexperimental studiessilicate meltsSpace and Planetary ScienceGeochemistry and Petrologyexperimental studies; helium; pressure; silicate melts; solubilityEarth and Planetary Sciences (miscellaneous)SolubilityDissolutionGeologyHelium
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Acid-Base Properties of 2:1 Clays. I. Modeling the Role of Electrostatics

2010

We present a theoretical investigation of the titratable charge of clays with various structural charge (sigma(b)): pyrophyllite (sigma(b) = 0 e x nm(-2)), montmorillonite (sigma(b) = -0.7 e x nm(-2)) and illite (sigma(b) = -1.2 e x nm(-2)). The calculations were carried out using a Monte Carlo method in the Grand Canonical ensemble and in the framework of the primitive model. The clay particle was modeled as a perfect hexagonal platelet, with an "ideal" crystal structure. The only fitting parameters used are the intrinsic equilibrium constants (pK(0)) for the protonation/deprotonation reactions of the broken-bond sites on the lateral faces of the clay particles, silanol, =SiO(-) + H(+) --=…

Base (chemistry)Mineralogy02 engineering and technologyengineering.material010402 general chemistry01 natural scienceschemistry.chemical_compoundElectrochemistryGeneral Materials ScienceCharging ProcessSpectroscopyPyrophyllitechemistry.chemical_classificationSurfaces and Interfaces021001 nanoscience & nanotechnologyCondensed Matter PhysicsElectrostatics0104 chemical sciences[ PHYS.PHYS.PHYS-CHEM-PH ] Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]MontmorillonitechemistryChemical engineeringvisual_artIlliteengineeringvisual_art.visual_art_mediumClay[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]0210 nano-technology
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Fracture stratigraphy and oil first migration in Triassic shales, Favignana Island, western Sicily, Italy

2021

This study aims at evaluating the control exerted by fracture stratigraphy and diagenetic processes on oil first migration through an outcropping, mixed carbonate-siliciclastic succession. The present work included results of sedimentological, paleontological, mineralogical, petrographic, structural, and microstructural analyses carried out on organic-rich shales exposed at the Favignana Island of Sicily, Italy. The analyses focus on Upper Triassic yellowish siltstones and greyish laminated dolomitic limestones, which form a 10's of m-thick succession exposed along the westernmost portion of the Sicilian fold-and-thrust belt. The studied succession deposited in a coastal lagoon associated t…

BeddingCarbonate platformOutcropStratigraphyFracture (mineralogy)GeochemistryGeologyBrittle deformationOceanographyDiagenesisPetrographyGeophysicsStratigraphySource rockUpper TriassicAnoxic coastal lagoonEconomic GeologyDiagenetic evolutionSicilyMixed carbonate-siliciclasticGeologyMarine and Petroleum Geology
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Fabric control on strain and rupture of heterogeneous shale samples by using a non-conventional mechanical test

2004

Abstract This work was a part of the preliminary stage of the ANDRA project on a deep-seated research laboratory for the feasibility study of long-term radioactive waste storage in the Callovo–Oxfordian argillites of the Eastern part of the Paris Basin. These rocks are bedded, their density is about 2.4, and they contain an average of 30% carbonates and 25% quartz. Thick (5 mm) sections from cores were put through a non-conventional device called CGI testcell (CGI: Centre de Geologie de l'Ingenieur, i.e. Engineering Geology Centre). The aim of this versatile device is to achieve plane deformation tests under compressive uniaxial loading together with controlled temperature and humidity cond…

BeddingLithologyMineralogyGeologyWeatheringengineering.materialBrittlenessShear (geology)Geochemistry and PetrologyengineeringPyriteOil shaleQuartzGeologyApplied Clay Science
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Mineralogical variability of Callovo-Oxfordian clays from the Paris Basin and the Subalpine Basin.

2006

High-resolution clay mineralogical data at the Middle/Upper Jurassic boundary from the French Subalpine Basin, the Jura Mountains and the Paris Basin (ANDRA boreholes) from Callovo-Oxfordian clayey deposits allow spatial and temporal terrigenous flux evolution to be considered over a period of 6 to 7 Myr. Recorded diachronisms of major mineralogical changes and complex clays distribution at the Paris Basin scale result to combined palaeogeographic/eustatic variations and climate input. In the French Subalpine Basin, mineralogical homogeneity confirms the burial diagenesis influence, but other terrigenous supplies must be involved in contrast to the Paris Basin domains. Volcanogenic clays (b…

Bentonites010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesCallovian[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/VolcanologyBiostratigraphyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesOxfordianPaleontologyPalaeovolcanismParis Basin[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgPhanerozoic[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesGlobal and Planetary ChangeTerrigenous sedimentDiagenesisClay minerals[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate actionClastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesSedimentary rockFrancePalaeogeographyGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Towards the development of a fossil bone geochemical standard: An inter-laboratory study

2007

Ten international laboratories participated in an inter-laboratory comparison of a fossil bone composite with the objective of producing a matrix and structure-matched reference material for studies of the bio-mineralization of ancient fossil bone. We report the major and trace element compositions of the fossil bone composite, using in-situ method as well as various wet chemical digestion techniques. For major element concentrations, the intra-laboratory analytical precision (%RSDr) ranges from 7 to 18%, with higher percentages for Ti and K. The %RSDr are smaller than the inter-laboratory analytical precision (%RSDR; 100% was found for the high field strength elements (Hf, Th, Zr, Nb). The…

Biogenic phosphateChemical compositionMineralogychemistry.chemical_elementFossil boneFossil bone/tooth010502 geochemistry & geophysics01 natural sciencesBiochemistryBone and BonesMass SpectrometryAnalytical ChemistryMatrix (chemical analysis)[CHIM.ANAL]Chemical Sciences/Analytical chemistryApatitesEnvironmental ChemistryAnimalsHigh field strengthInter-laboratoryChemical compositionSpectroscopy0105 earth and related environmental sciencesStrontiumChemistryRare-earth elementFossilsLasers010401 analytical chemistryTrace elementReproducibility of ResultsReference StandardsOrganophosphates0104 chemical sciencesTrace ElementsMetals Rare EarthReference material
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Plant Pigments: Properties, Analysis, Degradation

2005

Publisher Summary This chapter discusses the molecular structures, the general physicochemical properties of plant pigments, and the mechanisms involved in pigment degradation. The invasive and noninvasive methods used for pigment analysis, including the mechanisms involved in pigment degradation, are reviewed. The chapter presents different analytical methods that can be used to identify pigments. All the methods are invasive techniques that are time consuming and often expensive. To reduce sampling and analytical costs, and to speed up the analyses, noninvasive analytical procedures have been developed with the aim to characterize the pigment content of samples, and in the case of food pr…

Biological pigmentComplex matrixFood productsDeep knowledgePigment degradationDegradation (geology)Mineralogysense organsBiochemical engineeringBiology
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Possible functions of biomineralization of some Textulariid (Foraminifera) species of the Nw Iberian Margin

2016

The main goal of this work is to analyze the elemental composition of the test’s wall of some species/specimens of Textulariids (sub-class Subclass Textulariia), collected in surface sediments of the NW Iberian Margin. The elemental analyses was based on the Energy Dispersive Spectroscopy (EDS) on the Scanning Electron Microscope (SEM; Hitachi, S4100) of Textularia deltoidea, Textularia agglutinans, Sahulia conica, Karrerotextularia flintii, Siphotextularia heterostoma, Karreriella bradyi, Spiroplectammina sagittula and Arenoparrella mexicana . The elelemetal cocnentrations of the species wall were compared with the mineralogical composition (X-Ray diffraction) of the sediments of the stati…

Biomineralization010506 paleontologyElemental analysisEnergy-dispersive X-ray spectroscopyMineralogyTest (biology)010502 geochemistry & geophysics01 natural sciencesDeep seaSagittulaEDS[ SDE ] Environmental SciencesForaminiferaTextularialcsh:StratigraphyConica14. Life underwater0105 earth and related environmental scienceslcsh:QE640-699biologylcsh:QE1-996.5Wall compositionbiology.organism_classificationlcsh:GeologySEDIMENTOLOGIA MARINHAElemental analysisEnvironmental chemistrySEM[SDE]Environmental SciencesAgglutinated foraminifera
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Compartmentalization of gypsum and halite associated with cyanobacteria in saline soil crusts

2016

The interface between biological and geochemical components in surface crust of a saline soil was investigated using X-Ray Diffraction (XRD), and variable pressure scanning electron microscopy (SEM) in combination with Energy Dispersive X-ray Spectrometry (EDS). Mineral compounds such as halite and gypsum were identified crystallized around filaments of cyanobacteria. A total of 92 genera were identified from the bacterial community based on 16S gene pyrosequencing analysis. The occurrence of the gypsum crystals, their shapes and compartmentalization suggested that they separated NaCl from the immediate microenvironment of the cyanobacteria, and that some cyanobacteria and communities of su…

Biomineralization0301 basic medicineCyanobacteriaGypsumbiomineralisationSettore AGR/13 - Chimica Agraria030106 microbiologychemistry.chemical_elementMineralogySulfur bacteriaSodium ChlorideBiologyengineering.materialCyanobacteriaCalcium SulfateApplied Microbiology and BiotechnologyMicrobiologySoil03 medical and health sciencesX-Ray DiffractionSoil crustRNA Ribosomal 16SSoil MicrobiologyMineralSulfur CompoundsEcologyMedicine (all)biology.organism_classificationSulfurchemistrySettore AGR/14 - PedologiaMicroscopy Electron ScanningengineeringsulfobacteriaSoil crustHaliteSoil microbiologySaline soilBiomineralizationFEMS Microbiology Ecology
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