Search results for "recrystallization"

showing 10 items of 76 documents

Chemical variations in clay minerals of the Archaean Barberton Greenstone Belt (South Africa)

1996

Abstract Four rock profiles of shales, carbonates and greywacke-type sediments were sampled from the mafic compositional influenced sedimentary Fig Tree Group and from overlying, more felsic related, sedimentary Moodies Group of the Archaean Barberton Greenstone Belt in South Africa. Clay separates of forty sedimentary rocks were examined by XRD and SEM to study the mineralogical, chemical and morphological variations of the constitutive illite and chlorite. The clay minerals showed a significant K-enrichment in the illites and Mg- and Fe-depletions in the chlorites upwards the stratigraphic sequence. Three independent parameters influenced these variations: (1) a change in the origin of th…

Recrystallization (geology)FelsicLithologyGeochemistryGeologyGreenstone beltengineering.materialGeochemistry and PetrologyIlliteengineeringSedimentary rockMaficPetrologyClay mineralsGeologyPrecambrian Research
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Palaeoproterozoic ancestry of Pan-African high-grade granitoids in southernmost India: Implications for Gondwana reconstructions

2015

Abstract SHRIMP dating of magmatic zircons from granitoid gneisses and charnockites of the Trivandrum and Nagercoil Blocks in the granulite terrane of southernmost India yielded well-defined protolith emplacement ages between 1765 and ca. 2100 Ma and also document variable recrystallization and/or lead-loss during the late Neoproterozoic Pan-African event at around 540 Ma. Hf-in-zircon and whole rock Nd isotopic data suggest that the granitoid host rocks were derived from mixed crustal sources, and Hf–Nd model ages vary between 2.2 and 2.8 Ga. A gabbroic dyke, emplaced into a charnockite protolith and deformed together with it, only contained metamorphic zircon whose mean age of 542.3 ± 4.0…

Recrystallization (geology)GeochemistryMetamorphismCharnockiteGeologyKhondaliteGranuliteProtolithGeologyTerraneZirconGondwana Research
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Neoproterozoic ophiolite and related high-grade rocks of the Baikal–Muya belt, Siberia: Geochronology and geodynamic implications

2015

Abstract We report zircon for from ophiolitic and high-grade rocks of the Neoproterozoic Baikal–Muya belt of Siberia that occupies an arc-shaped area on the southeastern margin of the Siberian craton. It consists of arc-related plutonic, metavolcanic and metasedimentary rocks as well as fragmented ophiolites and high-grade metamorphic assemblages. Magmatic zircons from two plagiogranite dyke samples of the Mamakan ophiolite complex in the Sredne–Mamakan massif of the eastern Baikal–Muya belt yielded similar and concordant SHRIMP mean 206 Pb/ 238 U ages of 640.0 ± 4.1 and 650 ± 6 Ma, respectively, that reflect the time of dyke emplacement and from which we suggest an age of ca. 645 Ma as the…

Recrystallization (geology)GeochronologyGeochemistryMetamorphismGeologyGranuliteOphioliteProtolithGeologyEarth-Surface ProcessesZirconGneissJournal of Asian Earth Sciences
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Linking growth episodes of zircon and metamorphic textures to zircon chemistry: an example from the ultrahigh-temperature granulites of Rogaland (SW …

2003

In-situ U-Th-Pb analyses by ion-microprobe on zircon in intact textural relationships are combined with backscatter and cathodoluminescence imaging and trace element analyses to provide evidence for growth episodes of zircon. This approach helps: (a) to unravel the polymetamorphic history of aluminous migmatitic and granitoid gneisses of the regional contact aureole around the Rogaland anorthosite-norite intrusive complex; and (b) to constrain the age of M 2 ultrahigh-temperature (UHT) metamorphism and the subsequent retrograde M 3 event. All samples yield magmatic inherited zircon of c. 1035 Ma, some an additional group at c. 1050 Ma. This suggests that loss of Pb by volume diffusion in no…

Recrystallization (geology)Metamorphic rockGeochemistryMetamorphismGeologyOcean EngineeringIsogradMigmatiteGranuliteProtolithGeologyWater Science and TechnologyZirconGeological Society, London, Special Publications
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2016

Raman spectroscopic data were obtained for (Mg,Fe)2SiO4 samples during compression to 57 GPa. Single crystals of San Carlos olivine compressed hydrostatically above 41 GPa showed appearance of a new “defect” peak in the 820–840 cm−1 region associated with SiOSi linkages appearing between adjacent Embedded Image tetrahedra to result in five- or sixfold-coordinated silicate species. Appearance of this feature is accompanied by a broad amorphous background. The changes occur at lower pressure than metastable crystalline transitions of end-member Mg2SiO4 forsterite (Fo-I) into Fo-II and Fo-III phases described recently. We complemented our experimental study using density functional theory (DFT…

Recrystallization (geology)OlivineMaterials science010504 meteorology & atmospheric sciencesForsteriteengineering.material010502 geochemistry & geophysics01 natural sciencesSilicateAmorphous solidchemistry.chemical_compoundsymbols.namesakeCrystallographyGeophysicschemistryGeochemistry and PetrologyMetastabilitysymbolsengineeringCrystalliteRaman spectroscopy0105 earth and related environmental sciencesAmerican Mineralogist
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Influence of PVP/VA copolymer composition on drug–polymer solubility

2015

In this study, the influence of copolymer composition on drug-polymer solubility was investigated. The solubility of the model drug celecoxib (CCX) in various polyvinylpyrrolidone/vinyl acetate (PVP/VA) copolymer compositions (70/30, 60/40, 50/50 and 30/70 w/w) and the pure homopolymers polyvinylpyrrolidone (PVP) and polyvinyl acetate (PVA) was predicted at 25 °C using a thermal analysis method based on the recrystallization of a supersaturated amorphous dispersion (recrystallization method). These solubilities were compared with a prediction based on the solubility of CCX in the liquid monomeric precursors of PVP/VA, N-vinylpyrrolidone (NVP) and vinyl acetate (VA), using the Flory-Huggins …

Recrystallization (geology)PolymersChemistry PharmaceuticalPharmaceutical Science02 engineering and technologyFlory–Huggins solution theory030226 pharmacology & pharmacy03 medical and health scienceschemistry.chemical_compound0302 clinical medicineDrug StabilityPolymer chemistrymedicineVinyl acetateCopolymerSolubilityPolyvinyl acetatePolyvinylpyrrolidonePovidone021001 nanoscience & nanotechnologyMonomerSolubilitychemistryCelecoxibThermodynamicsPolyvinylsCrystallization0210 nano-technologyHydrophobic and Hydrophilic Interactionsmedicine.drugEuropean Journal of Pharmaceutical Sciences
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Disordered sodium alkoxides from powder data: crystal structures of sodium ethoxide, propoxide, butoxide and pentoxide, and some of their solvates

2021

The crystal structures of NaOEt, NaOPr, NaOBu and NaOAm (Am = amyl = pentyl) were determined from powder data. These compounds crystallize in an anti-PbO structure in the space groups P 21 m and P4/nmm. Additionally, solvates with the composition NaOEt·2EtOH, NaOPr·2PrOH, NaOiPr·5iPrOH and NaOtAm·tAmOH were synthesized, and their structures were determined from single crystals. They form interesting chain structures of different compositions and topologies.

Recrystallization (geology)Sodiumchemistry.chemical_elementAlcoholCrystal structure010402 general chemistry010403 inorganic & nuclear chemistry01 natural scienceschemistry.chemical_compoundsolvateBärnighausen treeMaterials Chemistryddc:530Alkylchemistry.chemical_classificationSodium ethoxideChemistryMetals and AlloysResearch PapersAtomic and Molecular Physics and Optics0104 chemical sciencesElectronic Optical and Magnetic MaterialsisopropanolCrystallographysodium alkoxide548PXRDddc:540Alkoxidepowder dataPowder diffraction
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High-Generation Amphiphilic Janus-Dendrimers as Stabilizing Agents for Drug Suspensions

2018

Pharmaceutical nanosuspensions are formed when drug crystals are suspended in aqueous media in the presence of stabilizers. This technology offers a convenient way to enhance the dissolution of poorly water-soluble drug compounds. The stabilizers exert their action through electrostatic or steric interactions, however, the molecular requirements of stabilizing agents have not been studied extensively. Here, four structurally related amphiphilic Janus-dendrimers were synthesized and screened to determine the roles of different macromolecular domains on the stabilization of drug crystals. Physical interaction and nanomilling experiments have substantiated that Janus-dendrimers with fourth gen…

Recrystallization (geology)huumeetPolymers and Plastics116 Chemical sciences02 engineering and technology01 natural sciencesdrugsContact angleMaterials ChemistryHUMAN LECTINSSurface plasmon resonanceta116chemistry.chemical_classificationChemistryBIOLOGICAL-MEMBRANES021001 nanoscience & nanotechnologyPROGRAMMABLE GLYCAN LIGANDSINDOMETHACIN317 PharmacyCLICK CHEMISTRYfarmaseuttinen kemia0210 nano-technologyHydrophobic and Hydrophilic InteractionsDendrimersSURFACEBioengineeringPoloxamer010402 general chemistryRSPOORLY SOLUBLE DRUGBiomaterialsHydrophobic effectSurface-Active AgentsSuspensionslääkeyhdisteetDendrimerAmphiphileGLYCODENDRIMERSOMESta216ta215AlkylMODULAR SYNTHESISWaterPoloxamerCombinatorial chemistry0104 chemical scienceslääkkeet1182 Biochemistry cell and molecular biologypharmaceutical nanosuspensionsCOMPLEX ARCHITECTURESBiomacromolecules
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Stable isotope composition and rare earth element content of vertebrate remains from the Late Cretaceous of northern Spain (Laño): did the environmen…

2003

Abstract Oxygen and carbon isotope measurements have been performed on phosphatic remains from faunal associations (dinosaurs, crocodiles, turtles and fish) of the Late Cretaceous continental and marine sediments from northern Spain (Basque Country). The environmental meaning of the oxygen isotope record in fossil reptiles is discussed on the basis of known paleoecology, modern fauna analogs, and apatite chemistry (rare earth elements (REE), CO32− and PO43− contents). Fossil remains in sandstones and argillites from two localities (Urria and Cuezva) have low (down to 16‰) and scattered δ18O(PO4,CO3) and δ13C values with REE patterns characterized by strong middle REE enrichments. These geoc…

Recrystallization (geology)δ13CStable isotope ratioPaleontologyOceanographyCretaceousIsotopes of oxygenDiagenesisPaleontologyIsotopes of carbonPaleoecologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Ice deformed in compression and simple shear: control of temperature and initial fabric

2012

AbstractLayered and polycrystalline ice was experimentally deformed in general shear involving axial compression (strain magnitude 0.5-17%) and simple shear (strain magnitude γ = 0.1-1.4). As the temperature is increased from -20°C to -2°C, there is at least a twofold enhancement in octahedral shear strain rate, which coincides with the onset of extensive dynamic recrystallization and a change in grain-size distribution at -15°C. Between -150C and -10°C the c-axis preferred orientation rapidly evolves with the initiation of two-maxima fabrics in shear zones. From -10°C to -2°C there is progressive evolution of a final c-axis pattern that is asymmetric with respect to the direction of shorte…

Shearing (physics)010506 paleontology010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectStrain hardening exponent01 natural sciencesAsymmetrySimple shearShear (geology)Dynamic recrystallizationGeotechnical engineeringCrystalliteShear zoneComposite materialGeology0105 earth and related environmental sciencesEarth-Surface Processesmedia_commonJournal of Glaciology
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