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. |
Amphibole | Chalcopyrite | Clay | Corundum | Diaspore | Garnet | Marcasite | Mica | Nickeline | None |
Pentlandite | Pyrite | Quartz | Serpentine | Spinel |
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 |
---|---|---|---|---|---|---|---|
Actinolite (*) | Amphibole | Ca2(Mg4.5-2.5Fe2+0.5-2.5)Si8O22(OH)2 | 1882 | 1878 | 0 | 3419 | |
Almandine (*) | Garnet | Fe2+3Al2(SiO4)3 | 1882 | 1878 | 0 | 2353 | |
Anthophyllite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 1882 | 1878 | 0 | 718 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 1882 | 1878 | 0 | 27198 | |
Chrysotile (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 1882 | 1878 | 0 | 951 | |
Goethite (*) | Diaspore | FeO(OH) | 1882 | 1878 | 0 | 7437 | |
Hematite (*) | Corundum | Fe2O3 | 1882 | 1878 | 0 | 14640 | |
Ilmenite (*) | Corundum | Fe2+Ti4+O3 | 1882 | 1878 | 0 | 5433 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 1882 | 1878 | 0 | 14899 | |
Marcasite (*) | Marcasite | FeS2 | 1882 | 1878 | 0 | 5674 | |
Pentlandite (*) | Pentlandite | (Ni,Fe)9S8 | 1882 | 1878 | 0 | 1512 | |
Phlogopite (*) | Mica Clay | KMg3(AlSi3O10)(OH)2 | 1882 | 1878 | 0 | 2273 | |
Pyrite (*) | Pyrite | FeS2 | 1882 | 1878 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 1882 | 1878 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 1882 | 1878 | 0 | 61156 | |
Tremolite (*) | Amphibole | Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 | 1882 | 1878 | 0 | 2562 | |
Violarite (*) | Spinel | FeNi2S4 | 1882 | 1878 | 0 | 380 |
Age ID | Locality Notes |
---|---|
Michelle_678 | Ni-Cu sulfides in komatiite |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
EG105_1057_016 | 1880 | 1880 | 1880 | Yes | Ni, Cu, Pt, Pd, Rh, Ir, Os, Ru | 212064 | Thompson Nickel Belt, Manitoba, Canada | Thompson | Begg et al. (2010) | 10.2113/econgeo.105.6.1057 | EG105_1057 | ||||||||||
Michelle_678 | 1882 | 1878 | 1880±5 | Age of deposit or general age of the metallogenic province | Ni, Cu | 15219 | Manibridge Mine, Thompson Nickel Belt, Manitoba, Canada | Manibridge | Hoatson et al. (2006) | 10.1016/j.oregeorev.2006.05.002 | OGR29_177 | See Table. 1 Global resources of nickel metal and ages of the major nickel sulfide deposits of the world. Age can refer to the age of a specific nickel sulfide deposit, or the general age of the metallogenic province containing nickel deposits that are similar to a dated deposit (e.g. 2705 Ma Komatiite-hosted deposits in the Eastern Goldfields Province). |
Sample | Source Locality | Reference URL |
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