Results 11 to 20 of about 2,325 (156)
Corona formation around monazite and xenotime during greenschist-facies metamorphism and deformation [PDF]
Epidote/allanite–fluorapatite coronae around monazite and xenotime are investigated in Permian pegmatites deformed under greenschist-facies conditions during Alpine tectonometamorphism in the Austroalpine basement, Eastern Alps.
F. Hentschel +4 more
doaj +4 more sources
Constraining the age of many types of ore deposits remains challenging because of the lack of radiogenic isotopes incorporated into common ore-forming minerals. The timing of pre-Caledonian-hosted Cu mineralization along the entire c.
Olierook, Hugo K. H. +31 more
core +4 more sources
Synthesis and properties of anhydrous rare-earth phosphates, monazite and xenotime: a review. [PDF]
This article summarizes the synthesis methods, crystal structures, and properties of anhydrous monazite and xenotime (REPO4) crystalline materials. For both monazite and xenotime, currently available Inorganic Crystal Structure Database data were used to
Chong S +5 more
europepmc +2 more sources
Nanoscale geochemistry and geochronology of xenotime: application to Earth sciences [PDF]
The PhD project titled ‘Nanoscale geochemistry and geochronology of xenotime: application to Earth sciences’ aims at identifying and understanding mineralogical mechanisms that impact geochronometers at the nanoscale. The project focuses on the nanoscale
Joseph, Cilva
core +1 more source
Shock deformation microstructures in xenotime from the Spider impact structure, Western Australia
The rare earth element-bearing phosphate xenotime (YPO4) is isostructural with zircon, and therefore it has been predicted that xenotime forms similar shock deformation microstructures. However, systematic characterization of the range of microstructures
Katarina Miljkovic (23287867) +5 more
core +2 more sources
Palaeoproterozoic prograde metasomatic-metamorphic overprint zones in Archean tonalitic gneisses, eastern Finland [PDF]
Several occurrences of coarse-grained kyanite rocks are exposed in the Archaean area of eastern Finland in zones trending predominantly northwest-southeast that crosscut all the Archaean structures and, locally, the Palaeoproterozoic metadiabase dykes ...
M. Pajunen, M. Poutiainen
doaj +1 more source
This paper reports on the preparation of xenotime-structured ceramics using the Spark Plasma Sintering (SPS) method. Y0.95Gd0.05PO4 (YPO4:Gd) phosphates were obtained using the sol-gel method.
Dmitriy A. Mikhaylov +11 more
doaj +1 more source
We have investigated the incorporation of the luminescent Eu3+ cation in different LnPO4 (Ln = Tb, Gd1−xLux, x = 0.3, 0.5, 0.7, 1) host phases. All samples were analyzed with powder X-ray diffraction (PXRD), Raman spectroscopy, and site-selective time ...
Henry Lösch +7 more
doaj +1 more source
Hydrothermal formation of heavy rare earth element (HREE)– xenotime deposits at 100 °C in a sedimentary basin [PDF]
Most rare earth element deposits form from magmatic fluids, but there have also been discoveries of heavy rare earth element (HREE)– enriched hydrothermal xenotime deposits within sedimentary basins.
David A. Banks +14 more
core +2 more sources
Phase Transformation Pathway of DyPO4 to 21.5 GPa
Interest in the deformation behavior and phase transformations of rare earth orthophosphates (REPO4s) spans several fields of science—from geological impact analysis to ceramic matrix composite engineering.
Jai Sharma +2 more
doaj +1 more source

