Search results for "QUARTZ"

showing 9 items of 239 documents

Bivergent extension in orogenic belts: The Menderes massif (southwestern Turkey)

1995

The central Menderes massif is characterized by an overall dome-shaped foliation pattern and a north-northeast-trending stretching lineation. The asymmetry of shear bands and quartz c-axis fabrics on either side of the structural dome demonstrate a top to the north-northeast shear sense in the northern part and a top to the south-southwest shear sense in the southern part of the submassif, i.e., a bivergent downdip movement. This suggests a symmetric collapse of the Alpine Menderes orogenic belt along two extensional shear zones. Conjugate shear bands and symmetric quartz c-axis fabrics in the east-trending transition zone demonstrate a coaxial deformation between the two extension domains.…

geographygeography.geographical_feature_categorySubductionContinental crustGeologyCrustMassifLineationPlate tectonicsShear (geology)PetrologyQuartzGeologySeismologyGeology
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Age, geodynamic setting, and mantle enrichment processes of a K-rich intrusion from the Meissen massif (northern Bohemian massif) and implications fo…

1997

The plutonic complex of the Meissen massif (northern margin of the Bohemian massif) comprises dioritic to mainly monzonitic and granitic rocks. The diorite to monzonite intrusions show major and trace element patterns typical for shoshonitic series. The chemical signatures of less crustally contaminated diorites are similar to arc-related shoshonitic rocks derived from continental lithospheric mantle (CLM) sources previously enriched by subduction of altered oceanic crust. Laser step heating 40Ar/39Ar analyses on actinolitic to edenitic amphiboles from geographically different occurrences of the monzonitic intrusion yielded concordant plateau ages as well as total gas ages ranging from 329.…

geographygeography.geographical_feature_categorySubductionGeochemistryQuartz monzoniteMassifDioriteBatholithOceanic crustGeneral Earth and Planetary SciencesInstitut für GeowissenschaftenEclogiteGeologyZirconGeologische Rundschau
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Creation of glass-characteristic point defects in crystalline SiO2 by 2.5 MeV electrons and by fast neutrons

2019

The support from M -ERANET project “MyND” is acknowledged. K.K. was partially supported by the Collaborative Research Project of Laboratory for Materials and Structures, Tokyo Institute of Technology . Visiting researcher support from Ecole Polytechnique, Palaiseau is appreciated. Mr. Olivier Cavani is thanked for the expert help with irradiations.

inorganic chemicalsLuminescenceMaterials science02 engineering and technologyCrystal structure01 natural sciencesMolecular physicsCrystal0103 physical sciences:NATURAL SCIENCES:Physics [Research Subject Categories]Materials ChemistryElectron beam processingIrradiationDangling bonds[PHYS]Physics [physics]010302 applied physicstechnology industry and agricultureDangling bondElectron irradiationQuartz021001 nanoscience & nanotechnologyCondensed Matter PhysicsCrystallographic defectAmorphizationNeutron temperatureElectronic Optical and Magnetic MaterialsAmorphous solidCeramics and CompositesSilica glass0210 nano-technologyJournal of Non-Crystalline Solids
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Determination of the Boron/Lead Ratio in Ceramic Materials Based on Electrochemical Quartz Crystal Microbalance

2004

A method for quantitatively determining the relationship boron/lead in ceramic materials is presented. It is based on the attachment of microsamples of ceramic frits to an electrochemical quartz crystal microbalance (EQCM). After a reductive deposition step in the � 0.25 to � 0.85 V (vs. AgCl/Ag) potential range, well-defined stripping peaks are recorded in 0.10 M NaCl plus 0.10 M mannitol. The deposition of boron and lead from suspensions of solid materials, and its subsequent oxidative dissolution can be monitorized at the EQCM. The quotient between the maximum mass gain and the corresponding charge passed enables for a direct quantitation of the boron/lead molar ratio in ceramic material…

inorganic chemicalsMaterials scienceStripping (chemistry)chemistry.chemical_elementQuartz crystal microbalanceCeramic materialsElectrochemistryAnalytical Chemistrychemistryvisual_artElectrochemistryvisual_art.visual_art_mediumDeposition (phase transition)CeramicBoronVoltammetryDissolutionElectroanalysis
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Novel supramolecular affinity materials based on (−)-isosteviol as molecular templates

2013

The readily available ex-chiral-pool building block (−)-isosteviol was combined with the C3-symmetric platforms hexahydroxytriphenylene and hexaaminotriptycene providing large and rigid molecular architectures. Because of the persistent cavities these scaffolds are very potent supramolecular affinity materials for head space analysis by quartz crystal microbalances. The scaffolds serve in particular as templates for tracing air-borne arenes at low concentration. The affinities of the synthesized materials towards different air-borne arenes were determined by 200 MHz quartz crystal microbalances.

inorganic chemicalstemplatesChemistryOrganic Chemistrytechnology industry and agricultureSupramolecular chemistryNanotechnologyaffinity materials(−)-IsosteviolCombinatorial chemistryAffinitiesFull Research Papersupramolecular chemistrytriphenylene ketalslcsh:QD241-441CrystalChemistryTemplatelcsh:Organic chemistrytriptyceneslcsh:Qlcsh:ScienceQuartzVolume concentrationBeilstein Journal of Organic Chemistry
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Yielding of a quartz sand from saturated to dry state

2020

The paper presents the results of an experimental work where we analyse the behaviour of an unsaturated quartz sand in a wide range of degree of saturation (from saturated to dry state). The possibility of anticipating the hydro-mechanical behaviour of the soils when they approach the dry state is fundamental in many areas. An extensive experimental program, including controlled-suction and constant water content oedometric tests, was carried out to deeply analyse the water retention behaviour and the relationship between the yield stress and suction (Loading-Collapse curve). All elasto-plastic models provide a monotonically increase of the yield stress with suction. This assumption implies…

lcsh:GE1-350021110 strategic defence & security studiesWork (thermodynamics)Materials scienceSuctionSettore ICAR/07 - GeotecnicabehaviorDegree of saturation0211 other engineering and technologies02 engineering and technologyGranular materialcompressionWater retentionYielding model unsaturated soilSoil watermedicineGeotechnical engineeringmedicine.symptomQuartzWater contentlcsh:Environmental sciences021101 geological & geomatics engineering
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Marbles of Sicily (Italy)

2008

marbles of Sicily limestone quartz arenite basaltSettore GEO/05 - Geologia Applicata
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Practical Strategies for Stable Operation of HFF-QCM in Continuous Air Flow

2013

Currently there are a few fields of application using quartz crystal microbalances (QCM). Because of environmental conditions and insufficient resolution of the microbalance, chemical sensing of volatile organic compounds in an open system was as yet not possible. In this study we present strategies on how to use 195 MHz fundamental quartz resonators for a mobile sensor platform to detect airborne analytes. Commonly the use of devices with a resonant frequency of about 10 MHz is standard. By increasing the frequency to 195 MHz the frequency shift increases by a factor of almost 400. Unfortunately, such kinds of quartz crystals tend to exhibit some challenges to obtain a reasonable signal-to…

quartz crystal microbalance; high fundamental frequency; allan deviation; turbulences; laminar flow element; acceleration sensitivity; temperature gradientSensors; Volume 13; Issue 9; Pages: 12012-12029
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Characteristics of Mesozoic fluvio-lacustrine formations of the western Central African Republic (Carnot Sandstones) by means of mineralogical and ex…

1990

Abstract The so-called Carnot Sandstones, Mesozoic fluvio-lacustrine detrital formation, which stretch over an area of more than 40 000 km 2 in the western part of the Central African Republic, are made of a succession of conglomerates, sandstones and argilites which can reach 300 m in thickness. Heavy mineral analyses and quartz exoscopic studies of this detrital material allow to understand the geology of these formations. The detrital material origin: heavy mineral distribution in the lower levels indicates mostly a meridional origin with a quantitatively poor peripheral supply. The importance of the transport: quartz exoscopic observations show that the main part of the detrital materia…

symbols.namesakePaleontologyHeavy mineralsymbolsErosionAlluviumContext (language use)Ecological successionMesozoicCarnot cycleQuartzGeologyJournal of African Earth Sciences (and the Middle East)
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