Search results for "Metamictization"

showing 9 items of 9 documents

Incomplete retention of radiation damage in zircon from Sri Lanka

2004

A suite of 18 zircon gemstones from placers in the Highland/Southwestern Complex, Sri Lanka, were subjected to a comprehensive study of their radiation damages and ages. The investigation included X-ray diffraction, Raman and PL spectroscopy, electron microprobe, PIXE and HRTEM analysis, as well as (U-Th)/He and SHRIMP U-Th-Pb age determinations. Zircon samples described in this study are virtually homogeneous. They cover the range from slightly metamict to nearly amorphous. Generally concordant U-Th-Pb ages averaging 555 ± 11 Ma were obtained. Late Ordovician zircon (U-Th)/He ages scattering around 443 ± 9 Ma correspond reasonably well with previously determined biotite Rb-Sr ages for rock…

PLOMBURANIUMGeochemistryMineralogy550 - Earth sciencesElectron microprobeengineering.materialDATATIONZIRCONIUMMetamictizationSTRONTIUMGeochemistry and PetrologyANALYSE SPECTRALERadiation damageZIRCONRadiogenic nuclideALTERATIONMETAMICTISATIONIRRADIATIONGeophysicsHomogeneousengineeringMICROSTRUCTURESri lankaBiotiteGeologyRADIOACTIVITEZircon
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15. Spectroscopic methods applied to zircon

2003

Natural and synthetic (pure and doped) zircon (ZrSiO4) have been studied with a variety of spectroscopic techniques. These techniques are based on different physical phenomena, for instance transitions between spin states of nuclei and electrons, energetic transitions of valence electrons, intra-molecular vibrations, or vibrations of atoms and molecular units in the lattice. All of the diverse spectroscopic techniques, however, have in common that they probe energy differences between a ground and excited states, mostly upon interaction of the mineral with incident radiation. Such interactions are not only determined by the excited elementary particles or molecules themselves but depend gre…

MetamictizationMaterials scienceValence (chemistry)Spin statesExcited stateElectronValence electronMolecular physicsZirconCharacterization (materials science)
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Spectroscopic methods applied to zircon

2003

Natural and synthetic (pure and doped) zircon (ZrSiO4) have been studied with a variety of spectroscopic techniques. These techniques are based on different physical phenomena, for instance transitions between spin states of nuclei and electrons, energetic transitions of valence electrons, intra-molecular vibrations, or vibrations of atoms and molecular units in the lattice. All of the diverse spectroscopic techniques, however, have in common that they probe energy differences between a ground and excited states, mostly upon interaction of the mineral with incident radiation. Such interactions are not only determined by the excited elementary particles or molecules themselves but depend gre…

WavelengthCrystallographyMetamictizationValence (chemistry)Spin statesGeochemistry and PetrologyChemistryExcited stateElectronValence electronMolecular physicsZirconReviews in Mineralogy and Geochemistry
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High Temperature Study of Metamict Steenstrupine

2010

Metamict minerals contain radioactive elements that degrade their crystal structure. Unlike other metamict minerals, annealing process under ambient pressure do not lead to direct recrystallization of steenstrupine.

MetamictizationMaterials scienceAnnealing (metallurgy)MetallurgyAnalytical chemistryRecrystallization (metallurgy)General Materials ScienceCrystal structureCondensed Matter PhysicsAtomic and Molecular Physics and OpticsAmbient pressureSolid State Phenomena
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Structural anisotropy and annealing-induced nanoscale atomic rearrangements in metamict titanite

2012

The structural state of metamict titanite was studied by Raman spectroscopy, complementary high-resolution transmission electron microscopy, and single-crystal X-ray diffraction. The results show that Raman scattering collected from metamict titanite is highly anisotropic, which is typical of single crystals. But surprisingly, the observed Raman-scattering dependence on the sample orientation is much more pronounced for heavily metamict than for weakly metamict titanite samples. These radiation-induced anisotropic effects are related to the specific atomic arrangements in metamict titanite. The Raman spectra collected in backscattering geometry from a plane nearly perpendicular to the chain…

Materials scienceAnnealing (metallurgy)Recrystallization (metallurgy)Crystal structureengineering.materialAmorphous solidMetamictizationsymbols.namesakeCrystallographyGeophysicsGeochemistry and PetrologyTitanitesymbolsengineeringRaman spectroscopyRaman scatteringAmerican Mineralogist
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Internal structures and dating of complex zircons from Meissen Massif monzonites, Saxony

1999

Abstract U–Pb zircon ages were determined for accessory zircons from two monzonites from the Meissen Massif (Northern Bohemian Massif, Germany) by SHRIMP ion microprobe. BSE and CL imaging revealed that the monzonite zircons, showing oscillatory growth zoning, often contain inherited cores. Raman microprobe measurements showed that zoned rims (U 277–1426 ppm, Th 144–910 ppm) are slightly disordered to moderately metamict whereas cores have a wide spectrum of structural states, from well-crystallized to highly metamict. The radionuclide (U+Th) content of cores varies from a few hundred to more than 20,000 ppm. SHRIMP ion probe measurements on zoned rims, interpreted as zircon growth during c…

geographygeography.geographical_feature_categoryProterozoicGeochemistryQuartz monzoniteGeologyMassifMetamictizationGeochemistry and PetrologyCarboniferousMagmaGeologyAmphiboleZirconChemical Geology
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Low-temperature Zr mobility: An in-situ synchrotron-radiation XRF study of the effect of radiation damage in zircon on the element release in $H_{2}O…

2006

The release of Zr, U, and Pb from nearly metamict zircon and its recrystallized analog and of Zr from fully crystalline and slightly radiation-damaged zircon in H 2 O + HCl ± SiO 2 fluids was investigated in situ at temperatures between 200 and 500 °C using a hydrothermal diamond-anvil cell and time-resolved synchrotron-radiation XRF analyses. Dissolution of nearly metamict zircon proceeded much faster than that of zircon with little or no radiation damage and resulted in a 1.5 to 2 log units higher Zr molality in 6 to 7 m HCl fluids. Extensive recrystallization of the almost fully amorphous material started at 260 to 300 °C in H 2 O + HCl, and at about 360 °C if quartz was added, and was c…

Aqueous solutionAnalytical chemistryRecrystallization (metallurgy)Mineralogy550 - Earth sciencesHydrothermal circulationAmorphous solidMetamictizationGeophysicsGeochemistry and Petrologyddc:550QuartzDissolutionGeologyZircon
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High Temperature Study of Metamict Rinkite

2013

Metamict minerals contain radioactive elements that degrade their crystal structure. During the annealing process under ambient pressure in argon atmosphere the sample of metamict rinkite recrystallizes to the primary crystalline form at 700°C. Further heating leads to the formation of a new crystalline phase.

MetamictizationMaterials scienceAnnealing (metallurgy)Analytical chemistryMineralogyGeneral Materials ScienceCrystal structureCondensed Matter PhysicsAtomic and Molecular Physics and OpticsArgon atmosphereRadioactive decayAmbient pressureSolid State Phenomena
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Long-term stability of alpha particle damage in natural zircon

2005

Abstract We report the first discovery of radiation damage haloes generated by alpha particles in zircon. Proterozoic zircon crystals from a potassium-rich leucogranite from the Adirondack Mountains, New York State, have interior regions that are generally low in actinide elements (UO 2  + ThO 2  ≤ 0.02 wt.%) but show a remarkable pattern of heterogeneous metamictisation. The degree of radiation damage in these regions is not uniformly low, as would be expected if it corresponded to the observed actinide distribution patterns and age of the crystals. Rather, radiation damage is significantly increased in the outermost micro-areas of the low-actinide regions. The additional radiation damage …

010504 meteorology & atmospheric sciencesMineralogyGeologyAlpha particleengineering.material010502 geochemistry & geophysics01 natural sciencesCrystallographic defectMolecular physicsLeucograniteMetamictizationGeochemistry and PetrologyRadiation damageengineeringFrenkel defectBiotiteGeology0105 earth and related environmental sciencesZirconChemical Geology
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