Search results for "lcsh:Mineralogy"

showing 8 items of 8 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
researchProduct

Two-Stage Origin of K-Enrichment in Ultrapotassic Magmatism Simulated by Melting of Experimentally Metasomatized Mantle

2019

The generation of strongly potassic melts in the mantle requires the presence of phlogopite in the melting assemblage, while isotopic and trace element analyses of ultrapotassic rocks frequently indicate the involvement of subducted crustal lithologies in the source. However, phlogopite-free experiments that focus on melting of sedimentary rocks and subsequent hybridization with mantle rocks at pressures of 1&ndash

Peridotitelcsh:Mineralogylcsh:QE351-399.2lamproites010504 meteorology & atmospheric sciencesLithologyultrapotassicTrace elementGeochemistryGeologyUltrapotassic igneous rocksengineering.material010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesK-enrichmentMantle (geology)MagmatismengineeringPhlogopiteSedimentary rockhigh-pressure experimentssubduction zonesGeology0105 earth and related environmental sciencesMinerals
researchProduct

Origin of Blue Sapphire in Newly Discovered Spinel–Chlorite–Muscovite Rocks within Meta-Ultramafites of Ilmen Mountains, South Urals of Russia: Evide…

2019

Blue sapphire of gem quality was recently discovered in spinel&ndash

Rb-Sr and Sm-Nd isotopylcsh:QE351-399.2010504 meteorology & atmospheric sciencescorundumMetamorphic rockGeochemistryMineralogyCorundumUral Mountainsengineering.material010502 geochemistry & geophysics01 natural sciencesMetasomatismblue sapphireLA-ICP-MSIlmenogorsky complex0105 earth and related environmental sciencesBasaltmeta-ultramafic rockslcsh:MineralogybiologymetasomatismMuscovitegeology.rock_typeGeologyGeotechnical Engineering and Engineering Geologybiology.organism_classificationengineeringSapphireNepheline syeniteLileGeologyMinerals
researchProduct

The Beginning of Western Greek Amphorae Production in Western Sicily: Archaeometric and Archaeological Studies on 6th–5th Centuries BCE Amphorae Manu…

2020

About 560 western Greek amphorae (6th–5th centuries BCE) re-used in enchytrismos burials were unearthed in the necropolis of the Dorian-Chalcidian colony of Himera in northwestern Sicily. Among the most striking issues is the determination of their geographical provenance. For this purpose, ceramic samples chipped from freshly broken surfaces of all the amphorae were first subdivided into macrofabrics by the use of a hand lens. Thereon, the samples were studied in accordance with standardized methods by the use of reflected light microscopy. Due to the special focus of our project on the characterization of Sicilian productions, a selection of amphorae which showed visible, macroscopic affi…

chemical analyseswestern Greek amphoraelcsh:Mineralogylcsh:QE351-399.2local productionSicilyHimerapetrographyMinerals
researchProduct

Effects of Briquetting and High Pyrolysis Temperature on Hydrolysis Lignin Char Properties and Reactivity in CO-CO2-N2 Conditions

2021

Carbonaceous reductants for pyrometallurgical applications are usually obtained from fossil-based sources. The most important properties of the reductants greatly depend on the application and the feeding of the reductant into the process. However, the mechanical strength, calorific value, fixed carbon content, and reactivity of the reductant are the properties that usually define the applicability of the reductant for different processes. The reactivity of the biochars is usually high in comparison to metallurgical coke, which may restrict the applicability of the biochar in reduction processes. One cause of the higher reactivity is the higher surface area of the biochars, which can be sup…

lcsh:Mineralogylcsh:QE351-399.2biomasshigh-temperature pyrolysisbiochar reactivityhydrolysis ligninbiocharMinerals
researchProduct

Corundum Anorthosites-Kyshtymites from the South Urals, Russia: A Combined Mineralogical, Geochemical, and U-Pb Zircon Geochronological Study

2019

Kyshtymites are the unique corundum-blue sapphire-bearing variety of anorthosites of debatable geological origin found in the Ilmenogorsky-Vishnevogorsky complex (IVC) in the South Urals, Russia. Their mineral association includes corundum-sapphire, plagioclase (An61&ndash

lcsh:QE351-399.2010504 meteorology & atmospheric sciencesGeochemistryMetamorphismengineering.material010502 geochemistry & geophysics01 natural sciencesIlmenogorsky-Vishnevogorsky complexAnorthositeUltramafic rockPlagioclasein situ LA-ICP-MS U-Pb zircon datingMetasomatismblue sapphire0105 earth and related environmental sciencessapphire geochemistrylcsh:MineralogyGeologyGeotechnical Engineering and Engineering GeologykyshtymitesanorthositesCarbonatiteengineeringProtolithGeologyZirconMinerals
researchProduct

An integrated analytical approach to define the compositional and textural features of mortars used in the underwater archaeological site of castrum …

2019

This paper aims to carry out an archaeometric characterization of mortar samples taken from an underwater environment. The fishpond of the archaeological site of Castrum Novum (Santa Marinella, Rome, Italy) was chosen as a pilot site for experimentation. The masonry structures reached the maximum thickness at the apex of the fishpond (4.70 m) and consisted of a concrete conglomerate composed of slightly rough stones of medium size bound with non-hydraulic mortar. After sampling, for a complete characterization of selected mortar fragments, different and complementary techniques (stereomicroscopy, polarizing optical microscopy, and X-ray powder diffraction analysis) were carried out in order…

lcsh:QE351-399.2restoration02 engineering and technologyhydraulic-type mortars010502 geochemistry & geophysics01 natural sciencesUnderwater cultural heritageUnderwaterPozzolanaSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.0105 earth and related environmental scienceslcsh:Mineralogybusiness.industrySampling (statistics)GeologyMasonryHydraulic-type mortars Minero-petrographic analysis Pozzolana Restoration021001 nanoscience & nanotechnologyGeotechnical Engineering and Engineering GeologyArchaeologyCharacterization (materials science)pozzolanaHomogeneousminero-petrographic analysisMortar0210 nano-technologybusinessGeology
researchProduct

Raman Investigations to Identify Corallium rubrum in Iron Age Jewelry and Ornaments

2016

International audience; During the Central European Iron Age, more specifically between 600 and 100 BC, red precious corals (Corallium rubrum) became very popular in many regions, often associated with the so-called (early) Celts. Red corals are ideally suited to investigate several key questions of Iron Age research, like trade patterns or social and economic structures. While it is fairly easy to distinguish modern C. rubrum from bone, ivory or shells, archaeologists are confronted with ancient, hence altered, artifacts. Due to ageing processes, archaeological corals lose their intensive red color and shiny surface and can easily be confused with these other light colored materials. We pr…

polyeneslcsh:QE351-399.2[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryDistribution networks02 engineering and technologyBiology010502 geochemistry & geophysics01 natural sciencescorals; shells; Raman spectroscopy; biogenic carbonates; carotenoids; polyenes; color fading; material degradation; archaeology[CHIM.ANAL]Chemical Sciences/Analytical chemistryArchaeological researchMaterial DegradationCorallium rubrumcoral0105 earth and related environmental sciencesmaterial degradationlcsh:MineralogyEcologycarotenoidscolor fadingGeologyOrnamentsarchaeology021001 nanoscience & nanotechnologyGeotechnical Engineering and Engineering Geologybiogenic carbonatesshellscoralsIron AgeRaman spectroscopy0210 nano-technology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyMinerals
researchProduct