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. |
None | Tourmaline |
Fluor-liddicoatite (*) |
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 |
---|---|---|---|---|---|---|---|
Fluor-liddicoatite (*) | Tourmaline | Ca(Li2Al)Al6(Si6O18)(BO3)3(OH)3F | 510 | 470 | 0 | 12 |
Age ID | Locality Notes |
---|---|
Alexandra-0289 | Outside pegmatite fields. |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Alexandra-0289 | 510 | 490 | 510–490 | U-Pb | Age of gabbro–granite | Yes | 22165 | Sangilen Upland, Tuva, Russia | West Sangilen | Zagorsky et al. (2014) | 10.1016/j.rgg.2014.01.008 | RGG55_237 | |||||||||
Alexandra-0290 | 508 | 488 | 508–488 | U-Pb | Age of granite | Yes | 22165 | Sangilen Upland, Tuva, Russia | South Sangilen | Zagorsky et al. (2014) | 10.1016/j.rgg.2014.01.008 | RGG55_237 | |||||||||
Alexandra-0097 | 501 | 487 | 494 ± 7 | U–Pb | Age of collision | Yes | 204951 | Sutlug River, Tuva, Russia | Sutlug River | Zagorsky et al. (2014) | 10.1016/j.rgg.2014.01.008 | RGG55_237 | |||||||||
Alexandra-0093 | 496 | 470 | 483 ± 13 | U–Pb | Age of collision | Yes | 49467 | Tastyg Spodumene Deposit, Tuva, Russia | Tastyg | Zagorsky et al. (2014) | 10.1016/j.rgg.2014.01.008 | RGG55_237 | spodumene pegmatites of the South Sangilen belt crystallized from melts in the presence of reduced C–O–H–N fluids—typical components of deep fluid flows (Kyznetsova, 2011; Kuznetsova and Prokof’ev, 2009). The detected features of the trace-element and fluid compositions of the pegmatites suggest the influence of mantle fluids on the mineralization, which was one of the factors contributing to the formation of the Tastyg large Li deposit (Kuznetsova, 2009, 2011). |
Sample | Source Locality | Reference URL |
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All locality data graciously provided by mindat.org
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