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. |
Aeschynite | Amorphous | Calcite | Fluorite | None | Not in a structural group | Pyrite |
Aeschynite-(Y) (*) | Calcite (*) | Fluorite (*) | Lusernaite-(Y) (*) | Opal (*) |
Pyrite (*) | Synchysite-(Ce) (*) |
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 |
---|---|---|---|---|---|---|---|
Aeschynite-(Y) (*) | Aeschynite | (Y,Ln,Ca,Th)(Ti,Nb)2(O,OH)6 | 40 | 35 | 0 | 141 | |
Calcite (*) | Calcite | Ca(CO3) | 40 | 35 | 0 | 27770 | |
Fluorite (*) | Fluorite | CaF2 | 40 | 35 | 0 | 9617 | |
Lusernaite-(Y) (*) | Not in a structural group | Y4Al(CO3)2(OH,F)11·6H2O | 40 | 35 | 0 | 2 | |
Opal (*) | Amorphous | SiO2·nH2O | 40 | 35 | 0 | 2994 | |
Pyrite (*) | Pyrite | FeS2 | 40 | 35 | 0 | 39462 | |
Synchysite-(Ce) (*) | None | CaCe(CO3)2F | 40 | 35 | 0 | 232 |
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 |
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All locality data graciously provided by mindat.org
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