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. |
Andalusite | Beryl | Chalcopyrite | Feldspar | Garnet | Nickeline | None | Not in a structural group | Pentlandite | Quartz |
Spinel |
Almandine (*) | Andalusite (*) | Chalcopyrite (*) | Cordierite (*) | Magnetite (*) |
Microcline (*) | Pentlandite (*) | Pyrrhotite (*) | Quartz (*) | Sillimanite (*) |
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 | 1847 | 1830 | 0 | 2353 | |
Andalusite (*) | Andalusite | Al2SiO5 | 1847 | 1830 | 0 | 1310 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 1847 | 1830 | 0 | 27198 | |
Cordierite (*) | Beryl | Mg2Al4Si5O18 | 1847 | 1830 | 0 | 1008 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 1847 | 1830 | 0 | 14899 | |
Microcline (*) | Feldspar | K(AlSi3O8) | 1847 | 1830 | 0 | 4924 | |
Pentlandite (*) | Pentlandite | (Ni,Fe)9S8 | 1847 | 1830 | 0 | 1512 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 1847 | 1830 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 1847 | 1830 | 0 | 61156 | |
Sillimanite (*) | Not in a structural group | Al2SiO5 | 1847 | 1830 | 0 | 1516 |
Age ID | Locality Notes |
---|---|
Michelle_646 | Basal Ni-Cu sulfides in mafic-ultramafic intrusion |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Cr-00006 | 1850 | 1850 | whole rock | Yes | Chromite | Cr | 146977 | Halls Creek Shire, Western Australia, Australia | EST PILBARA BLOCKS AND HALLS CREEK MOBILE ZONE, WESTERN AUSTRALIA | Sun et al. (1991) | 10.1016/0301-9268(91)90045-C | PR50_1 | |||||||||
EG105_1057_038 | 1830 | 1830 | 1830 | Ni, Cu, Pt, Pd, Rh, Ir, Os, Ru | 122909 | Sally Malay Ni Mine (Savannah), Mabel Downs Station, Halls Creek Shire, Western Australia, Australia | Sally Malay deposit | Begg et al. (2010) | 10.2113/econgeo.105.6.1057 | EG105_1057 | |||||||||||
Michelle_646 | 1847 | 1841 | 1844±3 | Age of deposit or general age of the metallogenic province | Ni, Cu | 122909 | Sally Malay Ni Mine (Savannah), Mabel Downs Station, Halls Creek Shire, Western Australia, Australia | Sally Malay | 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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