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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. |
| Chalcopyrite | Clinozoisite | Copper | Epidote | Gypsum | Molybdenite | None | Not in a structural group | Pyrite | Quartz |
| Sphalerite |
| Anhydrite (*) | Chalcopyrite (*) | Epidote (*) | Gold (*) | Gypsum (*) |
| Molybdenite (*) | Pyrite (*) | Quartz (*) | Sphalerite (*) |
| 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 |
|---|---|---|---|---|---|---|---|
| Anhydrite (*) | Not in a structural group | Ca(SO4) | 222.4 | 217.2 | 0 | 1588 | |
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 222.4 | 217.2 | 0 | 27198 | |
| Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 222.4 | 217.2 | 0 | 8173 | |
| Gold (*) | Copper | Au | 222.4 | 217.2 | 0 | 30554 | |
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 222.4 | 217.2 | 0 | 6890 | |
| Molybdenite (*) | Molybdenite | MoS2 | 222.4 | 219.6 | 0 | 5800 | |
| Pyrite (*) | Pyrite | FeS2 | 222.4 | 217.2 | 0 | 39462 | |
| Quartz (*) | Quartz | SiO2 | 222.4 | 217.2 | 0 | 61156 | |
| Sphalerite (*) | Sphalerite | ZnS | 222.4 | 217.2 | 0 | 21482 |
| 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Jen_0001477 | 201.3 | 200.5 | 200.9 ± 0.4 | U-Pb | age of mineralization | high | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | |||||
| Jen_0001479 | 194 | 193.2 | 193.6 ± 0.4 | U-Pb | age of mineralization | high | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | |||||
| Jen_0001492 | 201.1 | 200.1 | 200.6 ± 0.5 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001493 | 201.7 | 200.5 | 201.1 ± 0.6 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001494 | 203.7 | 202.7 | 203.2 ± 0.5 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001495 | 201.4 | 200.6 | 201 ± 0.4 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001496 | 201.2 | 199.6 | 200.4 ± 0.8 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001497 | 203.3 | 200.1 | 201.7 ± 1.6 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001498 | 204.5 | 202.9 | 203.7 ± 0.8 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001499 | 202.4 | 200.2 | 201.3 ± 1.1 | U-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001500 | 197.8 | 197.8 | 197.8 | Pb-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001501 | 209 | 209 | 209 | Pb-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001502 | 209.9 | 209.9 | 209.9 | Pb-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001503 | 205 | 205 | 205 | Pb-Pb | age of mineralization | zircon | JD05-279 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | date for the andesite tuff at Pine is comparable to the depositional age for the Duncan Member dated elsewhere in the Toodoggone district | ||||||
| Jen_0001528 | 194.1 | 192.5 | 193.3 ± 0.8 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001529 | 194.2 | 193.2 | 193.7 ± 0.5 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001530 | 195.1 | 193.1 | 194.1 ± 1 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001531 | 195.9 | 192.3 | 194.1 ± 1.8 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001532 | 194.7 | 192.3 | 193.5 ± 1.2 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001533 | 195.4 | 192.2 | 193.8 ± 1.6 | U-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001534 | 205 | 205 | 205 | Pb-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001535 | 192 | 192 | 192 | Pb-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001536 | 191 | 191 | 191 | Pb-Pb | age of mineralization | zircon | JD05-283 | Yes | Zircon | 203238 | Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Toodoggone District | Dickinson (2006) | MT2004_Dickinson | This age represents the cessation of magmatism in the Pine-Fin-Mex area. | ||||||
| Jen_0001474 | 218.4 | 217.2 | 217.8 ± 0.6 | U-Pb | age of mineralization | high | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. This represents the oldest magmatic event in the Pine-Fin-Mex area and also in the Toodoggone district. | ||||||
| Jen_0001475 | 222.4 | 219.6 | 221.0 ± 1.4 | Re-Os | age of mineralization | high | molybdenite | F05-06-103 | Molybdenite | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | ||||||
| Jen_0001480 | 219.8 | 216.2 | 218 ± 1.8 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001481 | 218.8 | 216.2 | 217.5 ± 1.3 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001482 | 218.6 | 217.2 | 217.9 ± 0.7 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001483 | 219 | 216 | 217.5 ± 1.5 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001484 | 226 | 206 | 216 ± 10 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001485 | 228 | 208 | 218 ± 10 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001486 | 222.6 | 213.2 | 217.9 ± 4.7 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001487 | 219.2 | 212.4 | 215.8 ± 3.4 | U-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001488 | 199 | 199 | 199 | Pb-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001489 | 220 | 220 | 220 | Pb-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001490 | 218 | 218 | 218 | Pb-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. | |||||||
| Jen_0001491 | 198 | 198 | 198 | Pb-Pb | age of mineralization | zircon | JD05-281 | Zircon | 209603 | Fin Cu-Au-Mo Deposit, Toodoggone River Area, Omenica Mining Division, British Columbia, Canada | Fin Cu-Au-Mo deposit | Dickinson (2006) | MT2004_Dickinson | Lead isotope values for sulphide minerals from main-stage veins indicate that magmatic-derived fluids interacted with country rocks and possibly other fluids. |
| Sample | Source Locality | Reference URL |
|---|---|---|
All locality data graciously provided by mindat.org
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