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Xenotime-(Y) from
Pyörönmaa pegmatite, Valkeakoski, Pirkanmaa, Finland


Locality type:Pegmatite
Classification
Species:Xenotime-(Y)
Formula:Y(PO4)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Xenotime-(Y) data
Locality Data:Click here to view Pyörönmaa pegmatite, Valkeakoski, Pirkanmaa, Finland
Data Identifiers
Mindat Occurrence Record ID:558482
Long-form Identifier:1:3:558482:6
GUID (UUID V4):c27d20ad-5522-4a9a-b8bc-4a06e914ce78
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
octahedron. Consequently, the formula for minasgeraisite-(Y) with the originally proposed Ca occupancy of the...some minerals in this group, including gadolinite-(Y) and datolite (Klaproth 1802, 1806), have been known...Černý & Ercit 2005), includes the gadolinite NYF (Nb-Y-F) sub-type family with a typical mineralogical association...Barringer Hill, Texas, USA (Landes 1932), and Pyörönmaa, Finland (Vorma et al. 1966). Gadolinite-subgroup...fluid-rich processes in pegmatites (Skodefjellet pegmatite, Svalbard; Majka et al. 2011), metagranites (Turčok
Journal (article/letter/editorial)
1922–1941, 2014 Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the...contributions of individual minerals to whole-rock Y and REE budget and to assess incorporation mechanisms...the essential reservoir for Y+REE in the Hlína granite accounting ~84% Y and 61% REE of the total whole-rock...important carrier of REE with ~13% Y and ~11% REE. At least ~21% REE and 1% Y were probably hosted by Th- and...rockforming minerals (quartz and feldspars) is low (~1% Y; 10% LREE; ~1% HREE) excluding Eu, which is hosted
 
Mineral and/or Locality  
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