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Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps
Replacement primary monazite apatite-allanite-epidote coronas eastern Alps
2012/3/31
Accessory monazite crystals in granites are commonly unstable during amphibolite fa-cies regional metamorphism and typically become mantled by newly formed apatite-allan-ite-epidote coronas. This dist...
The chemical composition of REE-Y-Th-U-rich accessory minerals in peraluminous granites of the Erzgebirge-Fichtelgebirge region, Germany, Part I: The monazite-(Ce)-brabantite solid solution series
chemical composition REE-Y-Th-U-rich accessory minerals peraluminous granites Erzgebirge-Fichtelgebirge region monazite-(Ce)-brabantite solid solution series
2012/3/31
eraluminous granites of the Erzgebirge-Fichtelgebirge, Germany, are hosts of various members of the monazite group of minerals that display an unprecedented compositional diversity. The Eibenstock S-t...
Monazite-xenotime thermobarometry: Experimental calibration of the miscibility gap in the binary system CePO4-YPO4
Monazite-xenotime thermobarometry Experimental calibration miscibility gap binary system CePO4-YPO4
2012/4/5
POweresynthesizedhydrothermallybetween300Cand10004Catpressuresof2,5,10,and15kbar.Experimentproductswereanalyzedbyelectronmicroprobe,andtheirlatticeparameterswrere?nedbyRietveldanalysisofXRDpowderpatte...
Experimental study of Th-bearing LaPO4 (780 °C, 200 MPa): Implications for monazite and actinide orthophosphate stability
Experimental study Th-bearing LaPO4 monazite actinide orthophosphate stability
2012/4/5
Acompletesolidsolutionhasbeenhydrothermallysynthesizedbetweenthetwoend-membersLaPOand(Ca Th )POat780Cand200MPa,indicatingthatthereisnolimitationintemperatureandpressureconditionscorrespondingtothoseof...