about
P1066
Hadean age for a post-magma-ocean zircon confirmed by atom-probe tomographyMagmatic δ18O in 4400–3900 Ma detrital zircons: A record of the alteration and recycling of crust in the Early ArcheanNano- and micro-geochronology in Hadean and Archean zircons by atom-probe tomography and SIMS: New tools for old mineralsLithium in Jack Hills zircons: Evidence for extensive weathering of Earth's earliest crust4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zirconCubic zirconia in >2370 °C impact melt records Earth's hottest crustA pressure-temperature phase diagram for zircon at extreme conditionsMicrostructural constraints on the mechanisms of the transformation to reidite in naturally shocked zirconShocked monazite chronometry: integrating microstructural and in situ isotopic age data for determining precise impact agesEmpirical constraints on shock features in monazite using shocked zircon inclusionsNanoscale deformation twinning in xenotime, a new shocked mineral, from the Santa Fe impact structure (New Mexico, USA)A terrestrial perspective on usingex situshocked zircons to date lunar impactsNew clues from Earth’s most elusive impact crater: Evidence of reidite in Australasian tektites from ThailandFRIGN zircon—The only terrestrial mineral diagnostic of high-pressure and high-temperature shock deformationEvidence for melting mud in Earth’s mantle from extreme oxygen isotope signatures in zirconTransformations to granular zircon revealed: Twinning, reidite, and ZrO2in shocked zircon from Meteor Crater (Arizona, USA)Microstructural dynamics of central uplifts: Reidite offset by zircon twins at the Woodleigh impact structure, AustraliaNanoscale records of ancient shock deformation: Reidite (ZrSiO4) in sandstone at the Ordovician Rock Elm impact craterReconciling early impacts and the rise of lifeEarly Proterozoic oceanic crust in the northern Colorado Front Range: Implications for crustal growth and initiation of basement faultsGeological Applications of Atom Probe Tomography: New Information from Old RocksPreservation of detrital shocked minerals derived from the 1.85 Ga Sudbury impact structure in modern alluvium and Holocene glacial depositsCorrelating planar microstructures in shocked zircon from the Vredefort Dome at multiple scales: Crystallographic modeling, external and internal imaging, and EBSD structural analysisIdentification and provenance determination of distally transported, Vredefort-derived shocked minerals in the Vaal River, South Africa using SEM and SHRIMP-RG techniquesLi isotopes and trace elements as a petrogenetic tracer in zircon: insights from Archean TTGs and sanukitoidsThe origin of high δ18O zircons: marbles, megacrysts, and metamorphismA record of ancient cataclysm in modern sand: Shock microstructures in detrital minerals from the Vaal River, Vredefort Dome, South AfricaPrimitive oxygen-isotope ratio recorded in magmatic zircon from the Mid-Atlantic RidgeSub-micron scale distributions of trace elements in zirconSHRIMP U-Pb and CAMECA 1280 oxygen isotope results from ancient detrital zircons in the Caozhuang quartzite, Eastern Hebei, North China Craton: Evidence for crustal reworking 3.8 Ga agoTi-in-zircon thermometry: applications and limitationsChapter 2.5 The Oldest Terrestrial Mineral Record: A Review of 4400 to 4000 Ma Detrital Zircons from Jack Hills, Western AustraliaRadiation damage and alteration of zircon from a 3.3 Ga porphyritic granite from the Jack Hills, Western AustraliaCorrelated microanalysis of zircon: Trace element, δ18O, and U–Th–Pb isotopic constraints on the igneous origin of complex >3900Ma detrital grainsInternal zoning and U–Th–Pb chemistry of Jack Hills detrital zircons: a mineral record of early Archean to Mesoproterozoic (4348–1576Ma) magmatismNanoscale occurrence of Pb in an Archean zirconSIMS microanalysis of the Strelley Pool Formation cherts and the implications for the secular-temporal oxygen-isotope trend of chertsThe Rietputs Formation in South Africa: A Pleistocene Fluvial Archive of Meteorite Impact Unique to the Kaapvaal CratonRole of Elastic Anisotropy in the Development of Deformation Microstructures in ZirconDetrital shocked zircon provides first radiometric age constraint (<1472 Ma) for the Santa Fe impact structure, New Mexico, USA
P50
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P50
description
Geologe
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geologist
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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A J Cavosie
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A. Cavosie
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A. J. Cavosie
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A.J. Cavosie
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Aaron Cavosie
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Aaron J Cavosie
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prefLabel
Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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Aaron J. Cavosie
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P244
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