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 | Beryl | Chalcopyrite | Clay | Garnet | Mica | Nickeline | None | Pentlandite | Pyrite |
Quartz | Spinel | Talc |
Almandine (*) | Anthophyllite (*) | Beryl (*) | Chalcopyrite (*) | Cummingtonite (*) |
Grunerite (*) | Magnetite (*) | Muscovite (*) | Pentlandite (*) | Pyrite (*) |
Pyrrhotite (*) | Quartz (*) | Talc (*) | Violarite (*) |
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 |
---|---|---|---|---|---|---|---|
Almandine (*) | Garnet | Fe2+3Al2(SiO4)3 | 2925 | 2917 | 0 | 2353 | |
Anthophyllite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 2925 | 2917 | 0 | 718 | |
Beryl (*) | Beryl | Be3Al2Si6O18 | 2925 | 2917 | 0 | 4286 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 2925 | 2917 | 0 | 27198 | |
Cummingtonite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 2925 | 2917 | 0 | 327 | |
Grunerite (*) | Amphibole | Fe2+2Fe2+5Si8O22(OH)2 | 2925 | 2917 | 0 | 223 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 2925 | 2917 | 0 | 14899 | |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 2925 | 2917 | 0 | 17380 | |
Pentlandite (*) | Pentlandite | (Ni,Fe)9S8 | 2925 | 2917 | 0 | 1512 | |
Pyrite (*) | Pyrite | FeS2 | 2925 | 2917 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 2925 | 2917 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 2925 | 2917 | 0 | 61156 | |
Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 2925 | 2917 | 0 | 3337 | |
Violarite (*) | Spinel | FeNi2S4 | 2925 | 2917 | 0 | 380 |
Age ID | Locality Notes |
---|---|
Michelle_619 | 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_037 | 2920 | 2920 | 2920 | Yes | Ni, Cu, Pt, Pd, Rh, Ir, Os, Ru | 267018 | Lake Johnston, Dundas Shire, Western Australia, Australia | Lake Johnston | Begg et al. (2010) | 10.2113/econgeo.105.6.1057 | EG105_1057 | ||||||||||
Michelle_619 | 2925 | 2917 | >2921±4 | Age of deposit or general age of the metallogenic province | Ni, Cu | 250497 | Maggie Hays Ni Mine, Lake Johnston, Dundas Shire, Western Australia, Australia | Maggie Hays | 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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