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2014
The Mukinbudin area, Western Australia, comprises a pegmatite field with pegmatite bodies classified as NYF-type [1]. Allanite-(Ce) has been found in Mukinbudin Feldspar Quarries in form of metamict masses. The allanite masses are round-shaped being up to tens of centimeters in diameter and show no distinct crystal faces.
Bermanec, Vladimir +4 more
openaire +2 more sources
The Mukinbudin area, Western Australia, comprises a pegmatite field with pegmatite bodies classified as NYF-type [1]. Allanite-(Ce) has been found in Mukinbudin Feldspar Quarries in form of metamict masses. The allanite masses are round-shaped being up to tens of centimeters in diameter and show no distinct crystal faces.
Bermanec, Vladimir +4 more
openaire +2 more sources
Allanite-(Ce) and epidotes in a feldspar deposit from Central Sardinia, Italy
1993Epidotes occur in albitites as light rare-earth element (LREE)-bearing accessory common phases.Chemical data suggest that there is a near complete solid-solution between epidote and allanite. In epidote-group minerals a pronounced zoning in REE was observed.
CARCANGIU G +3 more
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Allanite-(Ce) and Its Type Locality
Rocks & Minerals, 2006Petersen, Ole V. +2 more
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1996
Recent investigations have pointed out that epidotes and allanite-(Ce) are the main REE-bearing minerals in the albitites located in the granodiorite facies of Central Sardinia. Previous works on albitites hypothesize that they originated from Na and Mg-metasomatic alteration of granitoids.
Carcangiu G, Palomba M, Tamanini M
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Recent investigations have pointed out that epidotes and allanite-(Ce) are the main REE-bearing minerals in the albitites located in the granodiorite facies of Central Sardinia. Previous works on albitites hypothesize that they originated from Na and Mg-metasomatic alteration of granitoids.
Carcangiu G, Palomba M, Tamanini M
openaire +1 more source
Allanite-(Ce) ed epidoti a Terre Rare nelle albititi della Sardegna centrale (Italia)
1996Recent investigations have pointed out that epidotes and allanite-(Ce) are the main REE-bearing minerals in the albitites located in the granodiorite facies of Central Sardinia. Previous works on albitites hypothesize that they originated from Na and Mg-metasomatic alteration of granitoids.
Carcangiu Gianfranco +2 more
openaire +1 more source
Cr-rich Allanite-(Ce): the First Finding in Kimberlites
Mineralogical Journal, 2015openaire +1 more source
Allanite micro-geochronology: A LA-ICP-MS and SHRIMP U–Th–Pb study
Chemical Geology, 2007Daniela Rubatto +2 more
exaly