| 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 | 383 | 359 | 0 | 3419 | |
| Albite (*) | Feldspar | Na(AlSi3O8) | 383 | 359 | 0 | 8803 | |
| Anatase (*) | Not in a structural group | TiO2 | 383 | 359 | 0 | 2162 | |
| Andradite (*) | Garnet | Ca3Fe3+2(SiO4)3 | 383 | 359 | 0 | 1534 | |
| Antigorite (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 383 | 359 | 0 | 708 | |
| Arsenopyrite (*) | Arsenopyrite | FeAsS | 383 | 359 | 0 | 9052 | |
| Bismuthinite (*) | Stibnite | Bi2S3 | 383 | 359 | 0 | 1935 | |
| Calcite (*) | Calcite | Ca(CO3) | 383 | 359 | 0 | 27770 | |
| Cerussite (*) | Aragonite | Pb(CO3) | 383 | 359 | 0 | 4979 | |
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 383 | 359 | 0 | 27198 | |
| Chrysotile (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 383 | 359 | 0 | 951 | |
| Diopside (*) | Pyroxene | CaMgSi2O6 | 383 | 359 | 0 | 4135 | |
| Dolomite (*) | None | CaMg(CO3)2 | 383 | 359 | 0 | 9895 | |
| Fluorite (*) | Fluorite | CaF2 | 383 | 359 | 0 | 9617 | |
| Grossular (*) | Garnet | Ca3Al2(SiO4)3 | 383 | 359 | 0 | 1544 | |
| Hematite (*) | Corundum | Fe2O3 | 383 | 359 | 0 | 14640 | |
| Kaolinite (*) | Clay Kaolinite | Al2Si2O5(OH)4 | 383 | 359 | 0 | 5591 | |
| Ludwigite (*) | Ludwigite | Mg2Fe3+O2(BO3) | 383 | 359 | 0 | 134 | |
| Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 383 | 359 | 0 | 14899 | |
| Massicot (*) | None | PbO | 383 | 359 | 0 | 202 | |
| Microcline (*) | Feldspar | K(AlSi3O8) | 383 | 359 | 0 | 4924 | |
| Molybdenite (*) | Molybdenite | MoS2 | 383 | 359 | 0 | 5800 | |
| Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 383 | 359 | 0 | 17380 | |
| Orthoclase (*) | Feldspar | K(AlSi3O8) | 383 | 359 | 0 | 2349 | |
| Phlogopite (*) | Mica Clay | KMg3(AlSi3O10)(OH)2 | 383 | 359 | 0 | 2273 | |
| Pyrite (*) | Pyrite | FeS2 | 383 | 359 | 0 | 39462 | |
| Quartz (*) | Quartz | SiO2 | 383 | 359 | 0 | 61156 | |
| Rutile (*) | Rutile | TiO2 | 383 | 359 | 0 | 5614 | |
| Scheelite (*) | Scheelite | Ca(WO4) | 383 | 359 | 0 | 4894 | |
| Siderite (*) | Calcite | Fe(CO3) | 383 | 359 | 0 | 6417 | |
| Sphalerite (*) | Sphalerite | ZnS | 383 | 359 | 0 | 21482 | |
| Szaibélyite (*) | None | MgBO2(OH) | 383 | 359 | 0 | 87 | |
| Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 383 | 359 | 0 | 3337 | |
| Titanite (*) | Titanite | CaTi(SiO4)O | 383 | 359 | 0 | 4899 | |
| Tremolite (*) | Amphibole | Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 | 383 | 359 | 0 | 2562 | |
| Vesuvianite (*) | Vesuvianite | (Ca,Na)19(Al,Mg,Fe)13(SiO4)10(Si2O7)4(OH,F,O)10 | 383 | 359 | 0 | 1395 | |
| Wollastonite (*) | Wollastonite | CaSiO3 | 383 | 359 | 0 | 1247 |
| 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| sedexmvt-00097 | 383 | 359 | Late Devonian | host rock age | Yes | 157307 | Houjiangqiao Pb-Zn Deposit, Dao Co., Yongzhou, Hunan, China | Houhongqiao | Taylor et al. (2009) | USGSOFR2009_1297 |
All locality data graciously provided by mindat.org
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