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K Feldspar from
Conifer Road, Campfire Lake, Kenora District, Ontario, Canada


Locality type:Road
Classification
Species:'K Feldspar' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view K Feldspar data
Locality Data:Click here to view Conifer Road, Campfire Lake, Kenora District, Ontario, Canada
Data Identifiers
Mindat Occurrence Record ID:614296
Long-form Identifier:1:3:614296:4
GUID (UUID V4):ddafca63-c78c-4260-ade3-f314af99d82f
Nearest other occurrences of K Feldspar
32.8km (20.4 miles) Big Mack pegmatite, Paterson Lake Area, Kenora District, Ontario, Canada
80.6km (50.1 miles) Greer Lake feldspar quarry, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
80.8km (50.2 miles) Birse Lake Occurrence (Rose), Birse Lake, Lac-du-Bonnet area, Manitoba, Canada
80.9km (50.3 miles) GL 1 pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
81.1km (50.4 miles) GL-3 pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
81.2km (50.5 miles) Grace claim, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
82.3km (51.1 miles) GL-7 pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
82.3km (51.1 miles) Cleo pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
82.6km (51.3 miles) Annie Claim #3 pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
83.1km (51.6 miles) GL12A pegmatite, Greer Lake, Lac-du-Bonnet area, Manitoba, Canada
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
reheating event at 215±15 Ma (Lu et al. 1997) and K and Na metasomatism of the Finero Complex at 207 ...coarse-grained plagioclase unit (albite) with minor K-feldspar, and 4) quartz core with muscovite, garnet and...series of minerals (kaersutite for Mg, Si, Fe, Al, Na, K, rhodonite for Mn, apatite for P, Ca and F, sodalite...et al. (1998) and from the Conifer Road pegmatite in northwestern Ontario by Černý et al. (1998). Roda...environment, as proposed for the Conifer Road pegmatite, in northwestern Ontario, by Černý et al. (1998). We
 
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