Fluorapatite-hingganite-(Y) coronas as products of fluid-induced xenotime-(Y) breakdown in the Skoddefjellet pegmatite, Svalbard

Mineralogical Magazine

Volumn 75, Issue 1, 2011, Pages 159-167

  Majka, J ^a   Prsek J ^b   Budzyn B ^c   Bacik P ^d   Barker, A K ^a   Lodzinski M ^b  

^a UPPSALA UNIVERSITY   (Sweden)

^b AGH UNIVERSITY OF SCIENCE AND TECHNOLOGY   (Poland)

^c INSTITUTE OF GEOLOGICAL SCIENCES   (Poland)

^d Faculty of Natural Sciences   (Slovakia)

Author keywords

apatite; Caledonides; hingganite; pegmatite; Svalbard; xenotime

Indexed keywords

CALEDONIDES; HINGGANITE; PEGMATITE; SVALBARD; XENOTIME;

BEARINGS (STRUCTURAL); CALCIUM; DISSOLUTION; ERBIUM; FLUIDS; GADOLINIUM; MINERALOGY; PHOSPHATE MINERALS; SILICATE MINERALS; YTTERBIUM; APATITE;

GRANITE;

APATITE; BERYL; FLUID COMPOSITION; FLUORAPATITE; HOST ROCK; METASEDIMENT; METASOMATISM; PEGMATITE; XENOTIME;

ARCTIC; CALEDONIDES; SPITSBERGEN; SVALBARD; SVALBARD AND JAN MAYEN; WEDEL JARLSBERG LAND;

EID: 79959210794     PISSN: 0026461X     EISSN: 14718022     Source Type: Journal    
DOI: 10.1180/minmag.2011.075.1.159     Document Type: Article

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