Results 31 to 40 of about 1,919 (210)

Helium Diffusion in Natural Xenotime [PDF]

open access: yesGeochemistry, Geophysics, Geosystems, 2019
AbstractThe typically high U and Th contents of xenotime ([Y,HREE]PO4) make this accessory mineral a promising candidate for (U‐Th)/He thermochronometry if the 4He diffusivity can be constrained well enough to estimate its closure temperature. We report new results for two 4He step‐heating experiments on different‐sized fragments of a natural xenotime ...
Alyssa J. Anderson   +3 more
openaire   +1 more source

Geochemical characterisation of xenotime formation environments using U-Th [PDF]

open access: yes, 2017
Xenotime (YPO4) is a trace component in many metasedimentary and some igneous rocks, altered rocks and many hydrothermal ore assemblages, where it forms in response to a range of different processes from igneous crystallisation to low-temperature early ...
McNaughton, Neal, Rasmussen, B.
core   +1 more source

Comparative Binding Studies of the Chelators Methylolanthanin and Rhodopetrobactin B to Lanthanides and Ferric Iron. [PDF]

open access: yesChembiochem
The synthesis and the investigation of the lanthanide (Ln) and Fe‐binding properties of the putative lanthanophore methylolanthanin (MLL) and the siderophore rhodopetrobactin B (RPB B) are reported. While both chelators bind Lns, they unexpectedly precipitate with Lns under biologically relevant conditions and thereby challenge the proposed classic ...
Gutenthaler-Tietze SM   +9 more
europepmc   +2 more sources

An in-situ electron microscopy study of dual ion-beam irradiated xenotime-type ErPO$_4$ [PDF]

open access: yes, 2020
International audienceRare-earth phosphates adopting the xenotime (REPO 4 ; RE = Tb − Lu & Y, Sc) structure are proposed as a potential matrix for the confinement of minor actinides.
Dacheux, Nicolas   +6 more
core   +1 more source

Xenotime at the Nanoscale:U-Pb Geochronology and Optimisation of Analyses by Atom Probe Tomography [PDF]

open access: yes, 2021
Xenotime (YPO4) is an accessory phase common in low to high-temperature geological environments. Xenotime is an established geochronometer, though its small size, low modal abundance and textural complexity make it more difficult to analyse with ...
Saxey, David W.   +16 more
core   +1 more source

Spectrophotometric determination of erbium using kojic acid dye in different rare earth concentrates

open access: yesEgyptian Journal of Petroleum, 2018
A sensitive and selective spectrophotometric method was studied for the determination of erbium (Er) with kojic acid dye (koj) and cetylpyridinium chloride (CPC) as a cationic surfactant from Egyptian monazite and xenotime concentrates using third ...
A.A. Abdou   +4 more
doaj   +1 more source

Lanthanide Sulfate Recovery by Synergistic Dimethyl Ether and Na<sub>2</sub>SO<sub>4</sub> Fractional Crystallization. [PDF]

open access: yesChemSusChem
This work demonstrates synergistic lanthanide salt recovery from an aqueous magnet leachate to single ppm concentrations using Na2SO4 combined with dimethyl ether crystallization. This waste valorization process minimizes chemicals consumed and waste generated while maximizing the recovery of a critical material product. Lanthanides (Lns) are important
Tolbert C   +6 more
europepmc   +2 more sources

Decomposition of Xenotime by Sulfuric Process

open access: yesThe Journal of the Society of Chemical Industry, Japan, 1965
各種高純度材料として用いられる希土類元素中,イットリウム族化合物の分離精製法を検討するため本研究を行なった。第1段階として原鉱石の分解法(硫酸分解)について実験した。従来から用いられている方法,硫酸による浸漬法,水浸法について実験した結果,ゼノタイム粉末20gを1~2mlの水で湿潤し, 湿潤試料に濃硫酸60ml加え, 260~280℃ で2 時間加熱して分解すればイットリウム分はより効果的に抽出できた。ゼノタイム(50.0%Y2O3)粉末20gを上記の方法で分解し, 粗製酸化イットリウム(95~96%純度)9.5gが得られた。
Itiro TOYAMA, Tomizo NAKAMURA
openaire   +2 more sources

Radiogenic Pb in xenotime trapped in nanoscale inclusions of apatite during fluid alteration [PDF]

open access: yes, 2023
This study focuses on the low-temperature mineralogical response of xenotime, a phosphate mineral routinely used as a geochronometer, to fluid-assisted alteration.
Tacchetto, Tomaso   +19 more
core   +1 more source

Petrology and mineralogy of the Ulaan Del Zr-Nb-REE deposit, Lake Zone, Western Mongolia

open access: yesMongolian Geoscientist, 2020
The Ulaan Del deposit is located in the Lake Zone, Western Mongolia. In the area, middle-late Devonian alkali dykes of the Khalzan Complex are hosted in the middle-late Cambrian granodiorite-tonalite of the Togthohiinshil Complex. The alkali dykes of the
Sanjsuren Oyunbat
doaj   +1 more source

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