Search results for "Ilici"

showing 10 items of 238 documents

Fabrication of a Silicide Thermoelectric Module Employing Fractional Factorial Design Principles

2021

AbstractThermoelectric modules can be used in waste heat harvesting, sensing, and cooling applications. Here, we report on the fabrication and performance of a four-leg module based on abundant silicide materials. While previously optimized Mg2Si0.3Sn0.675Bi0.025 is used as the n-type leg, we employ a fractional factorial design based on the Taguchi methods mapping out a four-dimensional parameter space among Mnx-εMoεSi1.75−δGeδ higher manganese silicide compositions for the p-type material. The module is assembled using a scalable fabrication process, using a Cu metallization layer and a Pb-based soldering paste. The maximum power output density of 53 μW cm–2 is achieved at a hot-side temp…

fractional factorial designFabricationMaterials sciencesilicide thermoelectric modulebusiness.industryContact resistanceFractional factorial designCondensed Matter PhysicsThermoelectric materialsElectronic Optical and Magnetic MaterialsTaguchi methodschemistry.chemical_compoundThermoelectric generatorchemistryThermoelectric effectSilicideMaterials ChemistryOptoelectronicsElectrical and Electronic Engineeringbusiness
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Development of a data acquisition system using silicon detectors for PET applications

2016

Este trabajo describe el desarrollo de parte de la electr´onica elaborada para el diseño de un escáner de Tomografíıa de Emisión de Positrones (PET) denominado Petete. Dicho escáner debe identificar offline los eventos de coincidencia y utilizar la técnica de ToF (Time of Flight) para descartar el ruido de fondo, lo cual permite contribuir a la mejora de la relación señal-ruido (SNR) y por lo tanto al aumento de la calidad de las imágenes médicas. El principal uso del escáner PET será en la investigación para el estudio y prueba de diferentes detectores para la mejora de las prestaciones del escáner PET en términos de resolución espacial, tiempo de adquisición (lo cual implica la reducción …

física de partículasdetectores de silicio:FÍSICA [UNESCO]UNESCO::FÍSICAelectrónica
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Rhyolitic dykes of Paros Island, Cyclades

2005

Abstract The discovery of rhyolitic dykes from the NE part of the island of Paros is described here for the first time. The dykes that can be mapped for a length of ca. 1.1 km are striking about 6° and 38° NE. The width reaches up to 11m maximum. The rhyolitic rocks are porphyric with a fine-grained matrix of mainly feldspar, quartz, some biotites and opaques. K-feldspar, biotite and plagioclase occur as phenocrysts, and mafic-intermediate enclaves are common. At the chilled margin in contact to the gneissic country rocks the dykes are vitric. There, the enclaves have been preserved from contact reaction with the melt and alteration effects and show primary igneous minerals such as clinopyr…

geographyChilled margingeography.geographical_feature_categorybiologyGeochemistrySilicicengineering.materialFeldsparbiology.organism_classificationVolcanic rockvisual_artvisual_art.visual_art_mediumengineeringPlagioclasePhenocrystXenolithGeologyLile
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Sm–Nd, Rb–Sr and Pb–Pb dating of silicic carbonates from the early Archaean Barberton Greenstone Belt, South Africa

1998

Abstract Two silicic carbonate sequences occurring in the Onverwacht Group (OG) and the overlying Fig Tree Group (FTG) of the early Archaean Barberton Greenstone Belt, South Africa, contain silicified dolomites with primary structures and textures. They occur with volcanic rocks dated by single zircons. The associated Onverwacht felsic volcanics have an age of ∼3440–3416 Ma, whereas the Fig Tree volcanics are ∼3225 Ma old. Therefore, the depositional age of both sequences is between 3440 and 3225 Ma. Pb-isotopic data for different parts of a single OG whole rock sample form a linear array corresponding to a Pb–Pb age of 2632±99 Ma. Sm–Nd and Rb–Sr isotopes were analysed in four whole rock s…

geographyFelsicgeography.geographical_feature_categoryArcheanGeochemistrySilicicGeologyGreenstone beltSedimentary depositional environmentVolcanic rockchemistry.chemical_compoundchemistryGeochemistry and PetrologyGroup (stratigraphy)CarbonateGeologyPrecambrian Research
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Exceptional mobility of an advancing rhyolitic obsidian flow at Cordón Caulle volcano in Chile

2013

The emplacement mechanisms of rhyolitic lava flows are enigmatic and, despite high lava viscosities and low inferred effusion rates, can result in remarkably, laterally extensive (30 km) flow fields. Here we present the first observations of an active, extensive rhyolitic lava flow field from the 2011-2012 eruption at Cordón Caulle, Chile. We combine high-resolution four-dimensional flow front models, created using automated photo reconstruction techniques, with sequential satellite imagery. Late-stage evolution greatly extended the compound lava flow field, with localized extrusion from stalled, ~35 m-thick flow margins creating80 breakout lobes. In January 2013, flow front advance continu…

geographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLavaGeneral Physics and AstronomySilicicGeneral Chemistry010502 geochemistry & geophysics01 natural sciencesFlow fieldGeneral Biochemistry Genetics and Molecular BiologyFlow (mathematics)VolcanoRhyolitePetrologyGeology0105 earth and related environmental sciencesNature Communications
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The Devonian Stratigraphic Succession and Evolution of the Baltic Sedimentary Basin

2014

Facies analysis, biostratigraphic and taphonomic studies, a re-evaluation of signatures of worldwide events, and a new mathematical model of the Baltic sedimentary basin (BSB) have together enabled a better understanding to be gained of the development of the Devonian basins in the Baltic area. We have established four stages of basin evolution: (a) remnant basin stage (Lochkovian); (b) shallow epeiric basin stage, with mainly siliciclastic sedimentation (Pragian–early Frasnian); (c) shallow epeiric basin stage, with mainly carbonate sedimentation (Frasnian); and (d) infilling stage of the progressively narrowing shallow epeiric basin, with mixed sedimentation (Famennian).

geographyPaleontologygeography.geographical_feature_categoryStage (stratigraphy)Basin modellingFaciesLithostratigraphySiliciclasticSedimentary basinStructural basinDevonianGeology
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Characterization, provenance, and tectonic setting of Fig Tree greywackes from the Archaean Barberton Greenstone Belt, South Africa

1999

Abstract In this study, mineralogical and geochemical data, as well as Sr and Nd isotopic compositions of early Archaean greywackes from the Fig Tree Group are presented to provide further information about the evolution of the Barberton Greenstone Belt (BGB) of the Kaapvaal Craton, South Africa. The chemical data on the collected greywackes from the BGB suggest limited chemical modification of the source rocks. The Eu/Eu * anomaly is negative with an average value of 0.76 which is slightly higher than that of Eu-depleted crustal rocks (0.65). High Cr and Ni concentrations and a Cr/Ni ratio of about 1.6 indicate derivation from ultramafic sources without fractionation. Although rounded zirc…

geographyProvenancegeography.geographical_feature_categoryFelsicStratigraphyArcheanGeochemistryGeologyGreenstone beltCratonUltramafic rockIsland arcSiliciclasticGeologySedimentary Geology
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Partitioning between “wedge-top” river- and wave-dominated successions: an example from the late Tortonian — early Messinian Terravecchia Formation (…

2011

AbstractDetailed field sedimentological and facies analyses have been performed in the Terravecchia Formation cropping out in NW Sicily, in order to differentiate and describe, for the first time, wave- and river-dominated shallow-marine (deltaic) siliciclastic successions. The latter were deposited filling syntectonic basins, developed between the late Tortonian and early Messinian time, within the wedge-top depozone of the Sicilian Foreland Basin System. It has been observed that river-dominated successions, recording the deposition of small fan-deltas are characterized by fining- to coarsening upward, transgressive-regressive sequences which were mostly deposited filling relatively narro…

geographyQE1-996.5geography.geographical_feature_categoryOutcropterravecchia formationwedge-top depozoneGeologyEnvironmental Science (miscellaneous)Sedimentary basinLate Miocenelate miocenelanguage.human_languageforeland basin systemPaleontologyFacieslanguageGeneral Earth and Planetary SciencessicilySiliciclasticriver-dominated deltasTransgressivewave-dominated deltasSicilianForeland basinGeologyOpen Geosciences
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Phase petrology reveals shallow magma storage prior to large explosive silicic eruptions at Hekla volcano, Iceland

2017

Abstract Understanding the conditions that culminate in explosive eruptions of silicic magma is of great importance for volcanic hazard assessment and crisis mitigation. However, geological records of active volcanoes typically show a wide range of eruptive behavior and magnitude, which can vary dramatically for individual eruptive centers. In order to evaluate possible future scenarios of eruption precursors, magmatic system variables for different eruption types need to be constrained. Here we use petrological experiments and microanalysis of crystals to clarify the P – T – x state under which rhyodacitic melts accumulated prior to the H3 eruption; the largest Holocene Plinian eruption of…

geographyVulcanian eruptionExplosive eruptiongeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySilicicMagma chamber010502 geochemistry & geophysics01 natural sciencesGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyPumiceMagmaddc:550Earth and Planetary Sciences (miscellaneous)PhenocrystPetrologyGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Stratigraphy of the Neoproterozoic Damara Sequence in northwest Namibia: Slope to basin sub-marine mass-transport deposits and olistolith fields

2016

Abstract The Neoproterozoic Damara Sequence (>1000 m thick) is composed of siliciclastic and carbonate rocks that crop out in the Damara Belt, Namibia. In Damaraland (including the Vrede, Bethanis, Austerlitz and Toekoms farms), these rocks were deformed and metamorphosed under greenschist facies (biotite zone) conditions during the Damara Orogeny. The stratigraphy and paleoenvironments of the Damara Sequence rocks are debated by the scientific community. We use field data, including detailed 1:25,000 geological mapping, elaboration of stratigraphic profiles and observation of preserved primary structures, textures and composition, to identify lithofacies and lithofacies associations, and t…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAlluvial fanGeology010502 geochemistry & geophysics01 natural sciencesUnconformityOnlapPaleontologySequence (geology)Basement (geology)Geochemistry and PetrologyCarbonate rockThrust faultSiliciclasticGeology0105 earth and related environmental sciencesPrecambrian Research
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