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 |
---|---|---|---|---|---|---|---|
Aegirine (*) | Pyroxene | NaFe3+Si2O6 | 2000 | 1800 | 0 | 1022 | |
Almandine (*) | Garnet | Fe2+3Al2(SiO4)3 | 2000 | 1800 | 0 | 2353 | |
Arsenic (*) | Arsenic | As | 2000 | 1800 | 0 | 379 | |
Arsenopyrite (*) | Arsenopyrite | FeAsS | 2000 | 1800 | 0 | 9052 | |
Baryte (*) | Baryte | Ba(SO4) | 2000 | 1800 | 0 | 11547 | |
Bismuth (*) | Arsenic | Bi | 2000 | 1800 | 0 | 1966 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 2000 | 1800 | 0 | 27198 | |
Cordierite (*) | Beryl | Mg2Al4Si5O18 | 2000 | 1800 | 0 | 1008 | |
Cummingtonite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 2000 | 1800 | 0 | 327 | |
Diamond (*) | Diamond | C | 2000 | 1800 | 0 | 697 | |
Diopside (*) | Pyroxene | CaMgSi2O6 | 2000 | 1800 | 0 | 4135 | |
Galena (*) | Rocksalt | PbS | 2000 | 1800 | 0 | 24243 | |
Gold (*) | Copper | Au | 2000 | 1800 | 0 | 30554 | |
Graphite (*) | None | C | 2000 | 1800 | 0 | 2812 | |
Hedenbergite (*) | Pyroxene | CaFe2+Si2O6 | 2000 | 1800 | 0 | 741 | |
Ilmenite (*) | Corundum | Fe2+Ti4+O3 | 2000 | 1800 | 0 | 5433 | |
Kyanite (*) | Not in a structural group | Al2OSiO4 | 2000 | 1800 | 0 | 1507 | |
Lead (*) | Copper | Pb | 2000 | 1800 | 0 | 192 | |
Löllingite (*) | Löllingite | FeAs2 | 2000 | 1800 | 0 | 762 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 2000 | 1800 | 0 | 14899 | |
Maldonite (*) | None | Au2Bi | 2000 | 1800 | 0 | 88 | |
Marcasite (*) | Marcasite | FeS2 | 2000 | 1800 | 0 | 5674 | |
Moissanite (*) | Wurtzite | SiC | 2000 | 1800 | 0 | 57 | |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 2000 | 1800 | 0 | 17380 | |
Gersdorffite-Pa3 (*) | Pyrite | NiAsS | 2000 | 1800 | 0 | 767 | |
Phlogopite (*) | Mica Clay | KMg3(AlSi3O10)(OH)2 | 2000 | 1800 | 0 | 2273 | |
Pyrite (*) | Pyrite | FeS2 | 2000 | 1800 | 0 | 39462 | |
Pyrope (*) | Garnet | Mg3Al2(SiO4)3 | 2000 | 1800 | 0 | 341 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 2000 | 1800 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 2000 | 1800 | 0 | 61156 | |
Scheelite (*) | Scheelite | Ca(WO4) | 2000 | 1800 | 0 | 4894 | |
Siderite (*) | Calcite | Fe(CO3) | 2000 | 1800 | 0 | 6417 | |
Sphalerite (*) | Sphalerite | ZnS | 2000 | 1800 | 0 | 21482 | |
Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 2000 | 1800 | 0 | 3337 | |
Titanite (*) | Titanite | CaTi(SiO4)O | 2000 | 1800 | 0 | 4899 | |
Wollastonite (*) | Wollastonite | CaSiO3 | 2000 | 1800 | 0 | 1247 | |
Zircon (*) | Zircon | Zr(SiO4) | 2000 | 1800 | 0 | 5251 |
Age ID | Locality Notes |
---|---|
Giersdorf_00001020 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
Giersdorf_00001021 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
Giersdorf_00001022 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
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_00001022 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271947 | Michurinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Michurisnk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) | |||||||||
Giersdorf_00001020 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271956 | Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Severisnk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) | |||||||||
Giersdorf_00001021 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271945 | Vatutinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Vatutinsk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) |
Sample | Source Locality | Reference URL |
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