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K Feldspar from
Kožichovice II pegmatite, Kožichovice, Třebíč District, Vysočina Region, Czech Republic


Locality type:Pegmatite
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 Kožichovice II pegmatite, Kožichovice, Třebíč District, Vysočina Region, Czech Republic
Data Identifiers
Mindat Occurrence Record ID:1097437
Long-form Identifier:1:3:1097437:9
GUID (UUID V4):0
Nearest other occurrences of K Feldspar
4.5km (2.8 miles) ⓘKostelíček, Třebíč, Třebíč District, Vysočina Region, Czech Republic
5.6km (3.5 miles) ⓘBorovina, Třebíč, Třebíč District, Vysočina Region, Czech Republic
10.7km (6.6 miles) ⓘKojetice metamanganolite occurrence, Kojetice, Třebíč District, Vysočina Region, Czech Republic
14.3km (8.9 miles) ⓘPokojovice pegmatite, Pokojovice, Třebíč District, Vysočina Region, Czech Republic
19.3km (12.0 miles) ⓘU starého Čihadla pegmatite, Biskupice-Pulkov, Třebíč District, Vysočina Region, Czech Republic
24.3km (15.1 miles) ⓘPuklice pegmatites, Puklice, Jihlava District, Vysočina Region, Czech Republic
25.5km (15.8 miles) ⓘKřoví Quarry, Křoví, Žďár nad Sázavou District, Vysočina Region, Czech Republic
36.4km (22.6 miles) ⓘVěžná I pegmatite, Věžná, Žďár nad Sázavou District, Vysočina Region, Czech Republic
36.9km (22.9 miles) ⓘRožná deposit, Rožná, Žďár nad Sázavou District, Vysočina Region, Czech Republic
37.5km (23.3 miles) ⓘMoravské Bránice vesuvianite occurrence (České Bránice vesuvianite occurrence; Mährisch Branitz vesuvianite occurrence; Böhmisch Branitz vesuvianite occurrence), Moravské Bránice (České Bránice; Mährisch Branitz; Böhmisch Branitz), Brno-Country District, South Moravian Region, Czech Republic
References
Výravský, J, Škoda, R. & Novak, M. (2017) Kristiansenite, thortveitite and SCNbO4: Products of Ca-metasomatism of Sc-enriched columbite-(Mn) from NYF pegmatite Kožichovice II, Czech Republic. PEG2017. NGF Abstracts and Proceedings, 2017 (2): 169-172.
 
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