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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 |
|---|---|---|---|---|---|---|---|
| Anglesite (*) | Baryte | Pb(SO4) | 252 | 174 | 1 | 119812 | 2734 |
| Aragonite (*) | Aragonite | Ca(CO3) | 346.7 | 0 | 0 | 3250 | |
| Ashoverite (*) | None | Zn(OH)2 | 0 | 0 | 1 | 119812 | 6 |
| Baryte (*) | Baryte | Ba(SO4) | 346.7 | 0 | 4 | 119805,119809,119812,119814 | 11547 |
| Calcite (*) | Calcite | Ca(CO3) | 346.7 | 0 | 4 | 119812,119813,119816,119817 | 27770 |
| Cerussite (*) | Aragonite | Pb(CO3) | 252 | 174 | 1 | 119812 | 4979 |
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 346.7 | 0 | 2 | 119809,119816 | 27198 |
| Dolomite (*) | None | CaMg(CO3)2 | 346.7 | 0 | 1 | 119809 | 9895 |
| Enargite (*) | Enargite Wurtzite | Cu3AsS4 | 1 | 119816 | 910 | ||
| Ettringite (*) | Ettringite | Ca6Al2(SO4)3(OH)12·27H2O | 346.7 | 0 | 1 | 119812 | 93 |
| Fluorite (*) | Fluorite | CaF2 | 252 | 174 | 7 | 119805,119808,119809,119812,119813,119814,119816 | 9617 |
| Galena (*) | Rocksalt | PbS | 252 | 174 | 6 | 119805,119809,119812,119813,119816,119817 | 24243 |
| Goethite (*) | Diaspore | FeO(OH) | 346.7 | 0 | 1 | 119809 | 7437 |
| Greenockite (*) | Wurtzite | CdS | 346.7 | 0 | 2 | 119809,119812 | 717 |
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 346.7 | 0 | 2 | 119809,119812 | 6890 |
| Hawleyite (*) | Sphalerite | CdS | 346.7 | 0 | 1 | 119809 | 62 |
| Hematite (*) | Corundum | Fe2O3 | 346.7 | 0 | 0 | 14640 | |
| Hemimorphite (*) | Not in a structural group | Zn4(Si2O7)(OH)2·H2O | 0 | 0 | 1 | 119812 | 1689 |
| Hydrocerussite (*) | None | Pb3(CO3)2(OH)2 | 0 | 0 | 1 | 119812 | 201 |
| Hydrozincite (*) | None | Zn5(CO3)2(OH)6 | 0 | 0 | 2 | 119809,119812 | 1066 |
| Litharge (*) | None | PbO | 252 | 174 | 1 | 119812 | 139 |
| Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 346.7 | 0 | 0 | 14899 | |
| Marcasite (*) | Marcasite | FeS2 | 346.7 | 0 | 1 | 119809 | 5674 |
| Massicot (*) | None | PbO | 346.7 | 0 | 1 | 119812 | 202 |
| Millerite (*) | Millerite | NiS | 346.7 | 0 | 1 | 119809 | 1066 |
| Palygorskite (*) | Palygorskite Clay | (Mg,Al)2Si4O10(OH)·4H2O | 0 | 0 | 1 | 119812 | 306 |
| Pyrite (*) | Pyrite | FeS2 | 346.7 | 0 | 4 | 119809,119812,119813,119816 | 39462 |
| Pyrolusite (*) | Rutile | MnO2 | 346.7 | 0 | 1 | 119809 | 3106 |
| Pyromorphite (*) | Apatite | Pb5(PO4)3Cl | 346.7 | 0 | 1 | 119809 | 1725 |
| Pyrrhotite (*) | Nickeline | Fe7S8 | 346.7 | 0 | 0 | 9056 | |
| Quartz (*) | Quartz | SiO2 | 346.7 | 0 | 3 | 119809,119812,119816 | 61156 |
| Sidpietersite (*) | None | Pb2+4(S2O3)O2(OH)2 | 346.7 | 0 | 1 | 119812 | 3 |
| Smithsonite (*) | Calcite | Zn(CO3) | 0 | 0 | 3 | 119805,119809,119812 | 2473 |
| Sphalerite (*) | Sphalerite | ZnS | 252 | 174 | 4 | 119809,119812,119813,119816 | 21482 |
| Sulphur (*) | Sulphur | S | 252 | 174 | 1 | 119812 | 2045 |
| Sweetite (*) | None | Zn(OH)2 | 0 | 0 | 1 | 119812 | 4 |
| Weddellite (*) | Oxalate | Ca(C2O4)·2H2O | 0 | 0 | 2 | 119809,119812 | 32 |
| Wülfingite (*) | Cristobalite | Zn(OH)2 | 0 | 0 | 1 | 119812 | 5 |
| Wurtzite (*) | Wurtzite | ZnS | 346.7 | 0 | 2 | 119809,119816 | 372 |
| Age ID | Locality Notes |
|---|---|
| Michelle_551 | Near-surface occurrence of weddellite at a former limestone quarry. Weddellite forms as the oxalic acid from lichen interact with the limestone/calcite. |
| Michelle_727 | Ashover-Crich anticline is associated with the uplift of the Derbyshire Dome at 280 ma. The uplift exposed the Fallgate Volcanics, Matlock and Cawdor Limestone and Cawdor Shales of Visean age, and siltstone, mudstone and gritstone beds of Namurian age. |
| Michelle_807 | The Fallgate Volcanics is exposed by the uplift of the Derbyshire Dome. This formation was visible in the Milltown Quarry on the Northwest corner as the Fallgate Tuff but is currently buried beneath slurry from fluorite workings. |
| Michelle_808 | The Matlock and Crawdor Limestone are of Visean age. These formations host the Pb-Zn-Fluorite veins of Permo-Triassic to Jurassic age. The formations were exposed by the uplift of the Derbyshire Dome. |
| Michelle_809 | The Matlock and Crawdor Limestone are of Visean age. These formations host the Pb-Zn-Fluorite veins of Permo-Triassic to Jurassic age. The formations were exposed by the uplift of the Derbyshire Dome. |
| Michelle_810 | The Cawdor Shale |
| Michelle_811 | The Namurian age Ashover Grits include siltstone, mudstone and gritstone. |
| Michelle_812 | Pb-Zn-Fluorite mineral vein and chimney deposits in the Milltown Quarry are concentrated on the Southeastern flank of the Ashover-Crich anticline. Mineral veins (rakes) include Blackwell, Mill, Spencers, Great, Woodhead and Lomas. |
| Michelle_813 | The formation of zinc hydroxide minerals described here would require a highly alkaline oxidizing environment. Such an environment could have been caused locally by the leaching of calcined limestone, itself the result of lime burning or possibly of the older pre-gunpowder mining technique of fire-setting. A relationship between the formation of the zinc hydroxides and weddellite has not been ruled out. The paper refers this as the 'zinc hydroxide zone'. |
| 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_551 | 0 | 0 | Recent | Age of weddellite mineralization | high | Weddellite | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Weddellite occurs due to the interaction of surface lichen and limestone/calcite. | |||||||||
| Michelle_727 | 280 | 280 | 280 | Uplift of Derbyshire Dome | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Uplift of Derbyshire Dome | |||||||||||
| Michelle_807 | 346.7 | 330.9 | Visean | Stratigraphy | Age of Fallgate Volcanics | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of Fallgate Volcanics | ||||||||||
| Michelle_808 | 346.7 | 330.9 | Visean | Stratigraphy | Age of Matlock Limestone | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of Matlock Limestone | ||||||||||
| Michelle_809 | 346.7 | 330.9 | Visean | Stratigraphy | Age of Cawdor Limestone | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of Cawdor Limestone | ||||||||||
| Michelle_810 | 346.7 | 330.9 | Visean | Stratigraphy | Age of Cawdor Shales | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of Cawdor Shales | ||||||||||
| Michelle_811 | 326 | 313 | Namurian | Stratigraphy | Age of siltstone, mudstone and gritstone | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of siltstone, mudstone and gritstone | ||||||||||
| Michelle_812 | 252 | 174 | Permo-Triassic, Early Jurassic | Age of Mississippi Valley Type mineralization | Anglesite, Cerussite, Fluorite, Galena, Litharge, Sphalerite, Sulphur | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Age of Mississippi Valley Type mineralization | ||||||||||
| Michelle_813 | 0 | 0 | Anthropogenic | Possibly anthropogenic | high | Ashoverite, Hemimorphite, Hydrocerussite, Hydrozincite, Palygorskite, Smithsonite, Sweetite, Wulfingite | 1482 | Milltown Quarry, Milltown, Ashover, Derbyshire, England, UK | Milltown Quarry | Rust (1991) | UJMM10_14 | Mineralization is likely of post-mining age due to the calcination of limestone interacting with zinc from vein mineralization. The reference suggests an anthropogenic origin for mineralization of the zinc hydroxide zone. |
| Sample | Source Locality | Reference URL |
|---|---|---|
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