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 |
---|---|---|---|---|---|---|---|
Aikinite (*) | Meneghinite | CuPbBiS3 | 306 | 306 | 0 | 315 | |
Albite (*) | Feldspar | Na(AlSi3O8) | 306 | 306 | 0 | 8803 | |
Allanite-(Ce) (*) | Allanite Epidote | CaCe(Al2Fe2+)[Si2O7][SiO4]O(OH) | 306 | 306 | 0 | 706 | |
Baryte (*) | Baryte | Ba(SO4) | 306 | 306 | 0 | 11547 | |
Bismuth (*) | Arsenic | Bi | 306 | 306 | 0 | 1966 | |
Brannerite (*) | Brannerite | UTi2O6 | 306 | 306 | 0 | 248 | |
Brucite (*) | Brucite | Mg(OH)2 | 306 | 306 | 0 | 462 | |
Calcite (*) | Calcite | Ca(CO3) | 306 | 306 | 0 | 27770 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 306 | 306 | 0 | 27198 | |
Clausthalite (*) | Rocksalt | PbSe | 306 | 306 | 0 | 281 | |
Coffinite (*) | Zircon | U(SiO4)·nH2O | 306 | 306 | 0 | 566 | |
Covellite (*) | Covellite | CuS | 306 | 306 | 0 | 4165 | |
Dewindtite (*) | Phosphuranylite | H2Pb3(UO2)6O4(PO4)4·12H2O | 306 | 306 | 0 | 82 | |
Digenite (*) | Digenite | Cu1.8S | 306 | 306 | 0 | 1027 | |
Dolomite (*) | None | CaMg(CO3)2 | 306 | 306 | 0 | 9895 | |
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 306 | 306 | 0 | 8173 | |
Fluorite (*) | Fluorite | CaF2 | 306 | 306 | 0 | 9617 | |
Fourmarierite (*) | Schoepite | Pb1-xO3-2x(UO2)4(OH)4+2x·4H2O | 306 | 306 | 0 | 61 | |
Francevillite (*) | Fritzscheite | Ba(UO2)2(VO4)2·5H2O | 306 | 306 | 0 | 43 | |
Galena (*) | Rocksalt | PbS | 306 | 306 | 0 | 24243 | |
Gold (*) | Copper | Au | 306 | 306 | 0 | 30554 | |
Hematite (*) | Corundum | Fe2O3 | 306 | 306 | 0 | 14640 | |
Kasolite (*) | None | Pb(UO2)(SiO4)·H2O | 306 | 306 | 0 | 198 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 306 | 306 | 0 | 14899 | |
Marcasite (*) | Marcasite | FeS2 | 306 | 306 | 0 | 5674 | |
Molybdenite (*) | Molybdenite | MoS2 | 306 | 306 | 0 | 5800 | |
Monazite-(Ce) (*) | Monazite | Ce(PO4) | 306 | 306 | 0 | 945 | |
Mottramite (*) | Descloizite | PbCu(VO4)(OH) | 306 | 306 | 0 | 362 | |
Poubaite (*) | Tetradymite | PbBi2(Se,Te,S)4 | 306 | 306 | 0 | 6 | |
Pyrite (*) | Pyrite | FeS2 | 306 | 306 | 0 | 39462 | |
Pyrobelonite (*) | Descloizite | PbMn2+VO4(OH) | 306 | 306 | 0 | 21 | |
Quartz (*) | Quartz | SiO2 | 306 | 306 | 0 | 61156 | |
Raspite (*) | Raspite | Pb(WO4) | 306 | 306 | 0 | 26 | |
Rutile (*) | Rutile | TiO2 | 306 | 306 | 0 | 5614 | |
Siderite (*) | Calcite | Fe(CO3) | 306 | 306 | 0 | 6417 | |
Skippenite (*) | Tetradymite | Bi2Se2Te | 306 | 306 | 0 | 6 | |
Součekite (*) | Bournonite | CuPbBi(S,Se)3 | 306 | 306 | 0 | 6 | |
Uraninite (*) | Fluorite | UO2 | 306 | 306 | 0 | 2718 | |
Uranophane-α (*) | None | Ca(UO2)2(SiO3OH)2·5H2O | 306 | 306 | 0 | 890 | |
Watkinsonite (*) | Watkinsonite | PbCu2Bi4(Se,S)8 | 306 | 306 | 0 | 5 | |
Wittichenite (*) | None | Cu3BiS3 | 306 | 306 | 0 | 297 | |
Xenotime-(Y) (*) | Zircon | Y(PO4) | 306 | 306 | 0 | 939 | |
Zircon (*) | Zircon | Zr(SiO4) | 306 | 306 | 0 | 5251 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000991 | Uranium vein-type deposits located in the Otish Mountains basin (Quebec) are associated with strongly albitized doleritic dykes and sills. Two periods of mineralization were recognized. The first, contemporaneous with the albitization, consists of brannerite and uraninite. The second, separated from the previous by tectonic movements, is characterized by carbonate gangue (dolomite), and a complex association of selenides, tellurides and sulfides including: skippenite, watkinsonite, poubaite, soucekite, clausthalite, aikinite, wittichenite, molybdenite, pyrite, chalcopyrite, galena, digenite, covellite, electrum, native bismuth, and several unidentified bismuth selenides-tellurides. |
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_00000991 | 306 | 306 | 306 | The second cycle, which is weaker, produced pitchblende and coffinite mineralization in a calcite gangue. Its age is approximately 306 Ma and seems to correspondto the mineralizatione vent well known in other areas, as for example in the Athabasca basin | Calcite, Coffinite, Galena, Hematite, Marcasite, Pyrite | U | 16069 | Otish Mountains U Deposit, Otish Mts, Baie-James, Nord-du-Québec, Québec, Canada | Otish Mountains U Deposit | Johan et al. (1987) | CM25_625 | The age for the second mineralization event of the Otish Mountains which corresponds well to other nearby areas. |
Sample | Source Locality | Reference URL |
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