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| 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 |
|---|---|---|---|---|---|---|---|
| Actinolite (*) | Amphibole | Ca2(Mg4.5-2.5Fe2+0.5-2.5)Si8O22(OH)2 | 1 | 70876 | 3419 | ||
| Aegirine (*) | Pyroxene | NaFe3+Si2O6 | 40 | 35 | 1 | 70873 | 1022 |
| Aeschynite-(Y) (*) | Aeschynite | (Y,Ln,Ca,Th)(Ti,Nb)2(O,OH)6 | 40 | 35 | 2 | 70873,70874 | 141 |
| Albite (*) | Feldspar | Na(AlSi3O8) | 40 | 35 | 2 | 70871,70873 | 8803 |
| Allanite-(Ce) (*) | Allanite Epidote | CaCe(Al2Fe2+)[Si2O7][SiO4]O(OH) | 40 | 35 | 1 | 70873 | 706 |
| Anatase (*) | Not in a structural group | TiO2 | 40 | 35 | 2 | 70871,70873 | 2162 |
| Arsenopyrite (*) | Arsenopyrite | FeAsS | 40 | 35 | 1 | 70873 | 9052 |
| Baryte (*) | Baryte | Ba(SO4) | 40 | 35 | 1 | 70873 | 11547 |
| Beryl (*) | Beryl | Be3Al2Si6O18 | 40 | 35 | 1 | 70873 | 4286 |
| Brookite (*) | Brookite | TiO2 | 40 | 35 | 1 | 70873 | 700 |
| Calcite (*) | Calcite | Ca(CO3) | 40 | 35 | 2 | 70873,70874 | 27770 |
| Cannizzarite (*) | None | Pb8Bi10S23 | 40 | 35 | 1 | 70873 | 41 |
| Cerussite (*) | Aragonite | Pb(CO3) | 40 | 35 | 1 | 70873 | 4979 |
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 40 | 35 | 1 | 70873 | 27198 |
| Chamosite (*) | Chlorite Clay | (Fe2+,Mg,Al,Fe3+)6(Si,Al)4O10(OH,O)8 | 40 | 35 | 1 | 70873 | 577 |
| Chrysocolla (*) | Allophane | (Cu2-xAlx)H2-xSi2O5(OH)4·nH2O | 40 | 35 | 1 | 70873 | 3531 |
| Clinochlore (*) | Chlorite Clay | Mg5Al(AlSi3O10)(OH)8 | 1 | 70877 | 1756 | ||
| Clinozoisite (*) | Clinozoisite Epidote | Ca2Al3[Si2O7][SiO4]O(OH) | 1 | 70871 | 1025 | ||
| Cosalite (*) | None | Pb2Bi2S5 | 40 | 35 | 1 | 70873 | 344 |
| Datolite (*) | Gadolinite | CaB(SiO4)(OH) | 40 | 35 | 1 | 70873 | 498 |
| Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 40 | 35 | 1 | 70873 | 8173 |
| Fergusonite-(Y) (*) | Scheelite | YNbO4 | 40 | 35 | 1 | 70873 | 196 |
| Fluorite (*) | Fluorite | CaF2 | 40 | 35 | 2 | 70873,70874 | 9617 |
| Galena (*) | Rocksalt | PbS | 40 | 35 | 1 | 70873 | 24243 |
| Graphite (*) | None | C | 40 | 35 | 1 | 70873 | 2812 |
| Grossular (*) | Garnet | Ca3Al2(SiO4)3 | 1 | 70877 | 1544 | ||
| Hammarite (*) | Meneghinite | Cu2Pb2Bi4S9 | 40 | 35 | 1 | 70873 | 43 |
| Hellandite-(Y) (*) | Hellandite | (Ca,REE)4Y2Al 2(B4Si4O22)(OH)2 | 40 | 35 | 1 | 70873 | 18 |
| Hematite (*) | Corundum | Fe2O3 | 40 | 35 | 1 | 70873 | 14640 |
| Heulandite-Ca (*) | Heulandite | (Ca,Na,K)5(Si27Al9)O72·26H2O | 40 | 35 | 1 | 70873 | 246 |
| Heyrovskýite (*) | Lillianite | Pb6Bi2S9 | 40 | 35 | 1 | 70873 | 66 |
| Ilmenite (*) | Corundum | Fe2+Ti4+O3 | 40 | 35 | 1 | 70873 | 5433 |
| Kainosite-(Y) (*) | None | Ca2Y2(SiO3)4(CO3)·H2O | 40 | 35 | 1 | 70873 | 99 |
| Laumontite (*) | Not in a structural group | CaAl2Si4O12·4H2O | 40 | 35 | 2 | 70871,70873 | 1271 |
| Lusernaite-(Y) (*) | Not in a structural group | Y4Al(CO3)2(OH,F)11·6H2O | 40 | 35 | 1 | 70874 | 2 |
| Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 40 | 35 | 1 | 70873 | 14899 |
| Marcasite (*) | Marcasite | FeS2 | 40 | 35 | 1 | 70873 | 5674 |
| Molybdenite (*) | Molybdenite | MoS2 | 40 | 35 | 1 | 70873 | 5800 |
| Monazite-(Ce) (*) | Monazite | Ce(PO4) | 40 | 35 | 1 | 70873 | 945 |
| Opal (*) | Amorphous | SiO2·nH2O | 40 | 35 | 2 | 70873,70874 | 2994 |
| Prehnite (*) | Prehnite | Ca2Al(Si3Al)O10(OH)2 | 1 | 70877 | 1898 | ||
| Pyrite (*) | Pyrite | FeS2 | 40 | 35 | 3 | 70873,70874,70876 | 39462 |
| Quartz (*) | Quartz | SiO2 | 40 | 35 | 4 | 70871,70873,70876,70877 | 61156 |
| Rutile (*) | Rutile | TiO2 | 40 | 35 | 2 | 70871,70873 | 5614 |
| Sphalerite (*) | Sphalerite | ZnS | 40 | 35 | 1 | 70873 | 21482 |
| Stilbite-Ca (*) | Stilbite | NaCa4(Si27Al9)O72·28H2O | 40 | 35 | 1 | 70873 | 268 |
| Synchysite-(Ce) (*) | None | CaCe(CO3)2F | 40 | 35 | 2 | 70873,70874 | 232 |
| Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 1 | 70876 | 3337 | ||
| Titanite (*) | Titanite | CaTi(SiO4)O | 40 | 35 | 2 | 70871,70873 | 4899 |
| Tremolite (*) | Amphibole | Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 | 1 | 70876 | 2562 | ||
| Wulfenite (*) | Scheelite | PbMoO4 | 40 | 35 | 1 | 70873 | 1655 |
| Xenotime-(Y) (*) | Zircon | Y(PO4) | 40 | 35 | 1 | 70873 | 939 |
| Zincsilite (*) | Smectite-vermiculite | Zn3Si4O10(OH)2·4H2O (?) | 40 | 35 | 1 | 70873 | 4 |
| Zircon (*) | Zircon | Zr(SiO4) | 40 | 35 | 2 | 70871,70873 | 5251 |
| Zoisite (*) | Epidote | Ca2Al3[Si2O7][SiO4]O(OH) | 1 | 70871 | 1025 |
| Age ID | Locality Notes |
|---|---|
| Michelle_289 | Lusernaite-(Y) is found in late stage hydrothermal fractures related to the Alpine tectono metamorphic events. Seccarezze Quarry is an important quarry in the mining of the leucocratic orthogneiss known as "Luserna Stone." |
| 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Michelle_289 | 40 | 35 | 35-40 | Ar-Ar | Cooling age | phengite | 240992 | Seccarezze Quarries, Luserna Stone Quarries, Luserna Valley, Pellice Valley, Metropolitan City Of Turin, Piedmont, Italy | Seccarezze Quarries | Biagioni et al. (2013) | 10.2138/am.2013.4366 | AM98_1322 | Age of late stage fractures during the tertiary Alpine tectono metamorphic events. 35-40 ma is described as being the time that the greenschist facies overprinted an earlier eclogite facies during the exhumation of the Dora-Maira Massif and period of cooling after peak thermal conditions. |
| Sample | Source Locality | Reference URL |
|---|---|---|
All locality data graciously provided by mindat.org
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