Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org



The Mineral Evolution database is currently under development.

The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.


Locality Name:
Vítkov II, Tachov District, Plzeň Region, Czech Republic

Oldest recorded age at locality: 262
Youngest recorded age at locality: 258

mindat Locality ID: 188816
mindat URL: http://www.mindat.org/loc-188816.html

Tectonic Settings:

Total number of sublocalities beneath "Vítkov II, Tachov District, Plzeň Region, Czech Republic": 0
Total number of bottom-level sublocalities: 0

Latitude: 0°0'0"N
Longitude: 0°0'0"E
Decimal Degree (lat, lon): 0,0

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.

This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.

Elements at this locality, including sub-localities: Bi C Ca Cu Fe H K O P Pb S Se Si Ti U Zn 

Elements from minerals reported directly at this locality: Bi C Ca Cu Fe H K O P Pb S Se Si Ti U Zn 

Structural Groups for minerals in this locality: 
AutuniteBranneriteCalciteChalcopyriteCorundumNonePhosphuranylitePyriteQuartzRocksalt
SphaleriteTetradymiteZircon

17 IMA Minerals at location:
Autunite  (*)Becquerelite  (*)Brannerite  (*)Calcite  (*)Chalcopyrite  (*)
Clausthalite  (*)Coffinite  (*)Curite  (*)Galena  (*)Hematite  (*)
Nevskite  (*)Uranophane-β  (*)Phosphuranylite  (*)Pyrite  (*)Quartz  (*)
Sphalerite  (*)Uranophane-α  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Autunite  (*)AutuniteCa(UO2)2(PO4)2·10-12H2O26225801272
Becquerelite  (*)NoneCa(UO2)6O4(OH)6·8H2O262258092
Brannerite  (*)BranneriteUTi2O62622580248
Calcite  (*)CalciteCa(CO3)262258027770
Chalcopyrite  (*)ChalcopyriteCuFeS2262258027198
Clausthalite  (*)RocksaltPbSe2622580281
Coffinite  (*)ZirconU(SiO4)·nH2O2622580566
Curite  (*)NonePb3+x[(UO2)4O4+x(OH)3-x]2·2H2O262258051
Galena  (*)RocksaltPbS262258024243
Hematite  (*)CorundumFe2O3262258014640
Nevskite  (*)TetradymiteBi(Se,S)26225806
Uranophane-β  (*)NoneCa(UO2)2(SiO3OH)2·5H2O2622580144
Phosphuranylite  (*)PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4·8H2O2622580182
Pyrite  (*)PyriteFeS2262258039462
Quartz  (*)QuartzSiO2262258061156
Sphalerite  (*)SphaleriteZnS262258021482
Uranophane-α  (*)NoneCa(UO2)2(SiO3OH)2·5H2O2622580890



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000830The Vítkov II uranium deposit was mined from 1961 to 1988 and was ranked among medium-size uranium deposits in the Bohemian Massif. The total mine production of low-grade uranium ore (0.124wt.% U)was 3973 t U. This uranium deposit occurs in the central tectonic block of the Bor pluton. The deposit is evolved between two shear NNE–SSW zones. The shear zone 0–30 in the east is up to 5–7 m in thickness. Its infill consists of highly crushed altered rocks (albitised biotite granites and lamprophyres), quartz and carbonates. Rich accumulations of U-minerals often occur in its vicinity. The Vítkov shear zone (southern part of the Eastern shear zone evolved in area of the Zadní Chodov deposit) forms the western boundary of the deposit. It is very conspicuous and its thickness reaches several tens of meters. It is infilled by crushed and altered country rocks. The pennate NW–SE dislocations situated between the two shear zones are infilled by dyke biotite and two-mica granites and relatively rarely aplites. The occurrence of uranium mineralisation is controlled by NW-SE and NNW-SSE trending faults,which forma dense network of fractures and joints. The surrounding biotite granites are usually intensely altered. The ore bodies comprise U-minerals (coffinite, uraninite, brannerite) finely disseminated in the surrounding altered granitoids.


1 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Giersdorf_00000830262258260±2U-PbAge of uranium mineralization during the main ore stage of the Variscan eventuraninite   UraniniteBrannerite, Coffinite, UraniniteU188816Vítkov II, Tachov District, Plzeň Region, Czech RepublicVítkov II Uranium DepositRené (2017)10.1016/j.oregeorev.2016.09.033OGR81_188Age of uranium mineralization


SampleSource LocalityReference URL


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