A | This mineral is Anthropogenic. |
G | This mineral is directly dated. |
B | This mineral is reported as having this age. |
Y | This mineral is using an age reported as an element mineralization period. |
O | This mineral is using an age calculated from all data at the locality. |
R | The age displayed for this mineral originates from a different, non-child locality. |
P | The 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. |
Mineral name | Structural Groups | IMA Formula | Max Age (Ma) | Min Age (Ma) | # of Sublocalities containing mineral | LOCALITY IDs, not mindat ids | # of localities containing mineral |
---|---|---|---|---|---|---|---|
Albite (*) | Feldspar | Na(AlSi3O8) | 191 | 179 | 0 | 8803 | |
Anatase (*) | Not in a structural group | TiO2 | 191 | 179 | 0 | 2162 | |
Arsenic (*) | Arsenic | As | 191 | 179 | 0 | 379 | |
Arsenopyrite (*) | Arsenopyrite | FeAsS | 191 | 179 | 0 | 9052 | |
Athabascaite (*) | None | Cu5Se4 | 191 | 179 | 0 | 18 | |
Bassetite (*) | None | Fe2+(UO2)2(PO4)2(H2O)10 | 191 | 179 | 0 | 51 | |
Berzelianite (*) | None | Cu2-xSe (x ≈ 0.12) | 191 | 179 | 0 | 66 | |
Bismuth (*) | Arsenic | Bi | 191 | 179 | 0 | 1966 | |
Bismuthinite (*) | Stibnite | Bi2S3 | 191 | 179 | 0 | 1935 | |
Bornite (*) | None | Cu5FeS4 | 191 | 179 | 0 | 5516 | |
Brannerite (*) | Brannerite | UTi2O6 | 191 | 179 | 0 | 248 | |
Calciouranoite (*) | Wölsendorfite | (Ca,Ba,Pb,K,Na)U2O7·5H2O | 191 | 179 | 0 | 4 | |
Calcite (*) | Calcite | Ca(CO3) | 191 | 179 | 0 | 27770 | |
Chalcocite (*) | None | Cu2S | 191 | 179 | 0 | 5707 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 191 | 179 | 0 | 27198 | |
Clarkeite (*) | None | Na(UO2)O(OH)·nH2O | 191 | 179 | 0 | 18 | |
Clausthalite (*) | Rocksalt | PbSe | 191 | 179 | 0 | 281 | |
Clinochlore (*) | Chlorite Clay | Mg5Al(AlSi3O10)(OH)8 | 191 | 179 | 0 | 1756 | |
Cobaltite (*) | Cobaltite | CoAsS | 191 | 179 | 0 | 966 | |
Coffinite (*) | Zircon | U(SiO4)·nH2O | 191 | 179 | 0 | 566 | |
Covellite (*) | Covellite | CuS | 191 | 179 | 0 | 4165 | |
Cuprosklodowskite (*) | None | Cu(UO2)2(SiO3OH)2·6H2O | 191 | 179 | 0 | 58 | |
Dewindtite (*) | Phosphuranylite | H2Pb3(UO2)6O4(PO4)4·12H2O | 191 | 179 | 0 | 82 | |
Digenite (*) | Digenite | Cu1.8S | 191 | 179 | 0 | 1027 | |
Dolomite (*) | None | CaMg(CO3)2 | 191 | 179 | 0 | 9895 | |
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 191 | 179 | 0 | 8173 | |
Eskebornite (*) | Chalcopyrite | CuFeSe2 | 191 | 179 | 0 | 26 | |
Eucairite (*) | None | CuAgSe | 191 | 179 | 0 | 54 | |
Ferroselite (*) | Marcasite | FeSe2 | 191 | 179 | 0 | 51 | |
Florencite-(Ce) (*) | Alunite | CeAl3(PO4)2(OH)6 | 191 | 179 | 0 | 73 | |
Galena (*) | Rocksalt | PbS | 191 | 179 | 0 | 24243 | |
Geffroyite (*) | Pentlandite | (Cu,Fe,Ag)9Se8 | 191 | 179 | 0 | 10 | |
Hakite-(Hg) (*) | Tetrahedrite | Cu6(Cu4Hg2)Sb4Se13 | 191 | 179 | 0 | 12 | |
Hematite (*) | Corundum | Fe2O3 | 191 | 179 | 0 | 14640 | |
Hessite (*) | None | Ag2Te | 191 | 179 | 0 | 804 | |
Löllingite (*) | Löllingite | FeAs2 | 191 | 179 | 0 | 762 | |
Marcasite (*) | Marcasite | FeS2 | 191 | 179 | 0 | 5674 | |
Naumannite (*) | Not in a structural group | Ag2Se | 191 | 179 | 0 | 192 | |
Nickeline (*) | Nickeline | NiAs | 191 | 179 | 0 | 633 | |
Uranophane-β (*) | None | Ca(UO2)2(SiO3OH)2·5H2O | 191 | 179 | 0 | 144 | |
Proustite (*) | None | Ag3AsS3 | 191 | 179 | 0 | 733 | |
Pyrite (*) | Pyrite | FeS2 | 191 | 179 | 0 | 39462 | |
Quartz (*) | Quartz | SiO2 | 191 | 179 | 0 | 61156 | |
Rammelsbergite (*) | Löllingite | NiAs2 | 191 | 179 | 0 | 233 | |
Rutile (*) | Rutile | TiO2 | 191 | 179 | 0 | 5614 | |
Safflorite (*) | Löllingite | CoAs2 | 191 | 179 | 0 | 317 | |
Schröckingerite (*) | None | NaCa3(UO2)(SO4)(CO3)3F·10H2O | 191 | 179 | 0 | 128 | |
Silver (*) | Copper | Ag | 191 | 179 | 0 | 5186 | |
Skutterudite (*) | Skutterudite Perovskite | CoAs3 | 191 | 179 | 0 | 531 | |
Soddyite (*) | None | (UO2)2(SiO4)(H2O)2 | 191 | 179 | 0 | 44 | |
Sphalerite (*) | Sphalerite | ZnS | 191 | 179 | 0 | 21482 | |
Stützite (*) | None | Ag5-xTe3 (x = 0.24-0.36) | 191 | 179 | 0 | 92 | |
Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 191 | 179 | 0 | 5317 | |
Thorite (*) | Zircon | Th(SiO4) | 191 | 179 | 0 | 1006 | |
Tiemannite (*) | Sphalerite | HgSe | 191 | 179 | 0 | 83 | |
Tsumoite (*) | Tetradymite | BiTe | 191 | 179 | 0 | 100 | |
Umangite (*) | None | Cu3Se2 | 191 | 179 | 0 | 71 | |
Uraninite (*) | Fluorite | UO2 | 191 | 179 | 0 | 2718 | |
Uranocircite-II (*) | None | Ba(UO2)2(PO4)2·10H2O | 191 | 179 | 0 | 89 | |
Uranosphaerite (*) | None | Bi(UO2)O2(OH) | 191 | 179 | 0 | 18 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000829 | The Zadní Chodov uranium deposit was mined from 1952 to 1992 and was ranked among medium-size uranium deposits in the Bohemian Massif. The totalmine production of low-grade uranium ore (0.195 wt.% U) was 4151 t U. The deposit, which is located in the northern tectonic block of the Bor pluton, was investigated by mine workings down to levels of 1250m in a length of over 2.5 km. The contact with the Moldanubian high-grade metasediments is tectonic, comprising several parallel shear structures to the Zadní Chodov fault,which forms the western boundary of the Bor pluton. Migmatised biotite paragneisses of the Moldanubian Varied Group predominate and they contain intercalations of quartzites, amphibolites, calc-silicate rocks and crystalline limestones. Dykes and bodies of amphibole-biotite tonalites and biotite granites cut the paragneisses. Aplite, pegmatite and lamprophyre dykes occur but are less frequent and are particularly developed above and below large shear zones. Uranium mineralisation is associated with the N-S trending zones of the Zadní Chodov fault in areas of their intersection with NW-SE trending fault structures, which form a NW continuation of the Central fault. The Zadní Chodov shear zone has been verified in an extent exceeding 20 km, its thickness in the middle part reaches 500m, and the dip is 50–75° to the east. This dislocation passes northwards into the Eastern shear zone of the Zadní Chodov deposit. The infill of the shear zones consists of intensely altered and crushed rocks with chlorite-rich and/or clay-mineral-rich assemblages. Uranium mineralisation was concentrated into three shear zones |
Excel ID | Max Age (Ma) | Min Age (Ma) | Age as listed in reference | Dating Method | Age Interpret | Prioritized? | Sample Source | Sample Num | Run Num | Age from other Locality | Dated Mineral | Minerals explicitely stated as having this age | Age applies to these Elements | MinDat Locality ID | Dated Locality (Max Age) | Location as listed in reference | Reference | Reference DOI | Reference ID | Age Notes | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Giersdorf_00000829 | 191 | 179 | 185±6 | U-Pb | Mesozoic recrystallization of brannerite during the main ore stage. | brannerite | Brannerite | Brannerite, Coffinite, Uraninite | U | 106091 | Zadní Chodov (Hinterkotten), Planá U Mariánských Lázní, Tachov District, Plzeň Region, Czech Republic | Zadní Chodov Uranium Deposit | René (2017) | 10.1016/j.oregeorev.2016.09.033 | OGR81_188 | Age of uranium mineralization |
Sample | Source Locality | Reference URL |
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