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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 | Compreignacite | Fluorite | Gypsum | None | Tetrahedrite | Zippeite |
| 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 |
|---|---|---|---|---|---|---|---|
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 370 | 290 | 0 | 27198 | |
| Compreignacite (*) | Compreignacite | K2(UO2)6O4(OH)6·7H2O | 0 | 0 | 0 | 27 | |
| Cuprosklodowskite (*) | None | Cu(UO2)2(SiO3OH)2·6H2O | 0 | 0 | 0 | 58 | |
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 543 | 0 | 0 | 6890 | |
| Marécottite (*) | None | Mg3O6(UO2)8(SO4)4(OH)2·28H2O | 0 | 0 | 0 | 10 | |
| Pseudojohannite (*) | None | Cu3(OH)2[(UO2)4O4(SO4)2]·12H2O | 0 | 0 | 0 | 10 | |
| Rabejacite (*) | None | Ca2[(UO2)4O4(SO4)2](H2O)8 | 0 | 0 | 0 | 11 | |
| Sejkoraite-(Y) (*) | Zippeite | Y2[(UO2)8O6(SO4)4(OH)2]·26H2O | 0 | 0 | 0 | 2 | |
| Tennantite-(Fe) (*) | Tetrahedrite | Cu6(Cu4Fe2)As4S13 | 543 | 0 | 0 | 1803 | |
| Tyuyamunite (*) | None | Ca(UO2)2(VO4)2·5-8H2O | 0 | 0 | 0 | 628 | |
| Uraninite (*) | Fluorite | UO2 | 370 | 290 | 0 | 2718 | |
| Uranopilite (*) | None | (UO2)6(SO4)O2(OH)6·14H2O | 0 | 0 | 0 | 94 | |
| Zippeite (*) | Zippeite | K2[(UO2)4(SO4)2O2(OH)2](H2O)4 | 0 | 0 | 0 | 175 |
| Age ID | Locality Notes |
|---|---|
| Michelle_541 | Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall |
| Michelle_542 | Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall |
| Michelle_543 | Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall |
| Michelle_544 | Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall |
| 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_541 | 0 | 0 | 0 | Brochantite, Compreignacite, Cuprosklodowskite, Jarosite, Johannite, Marecottite, Metazeunerite, Rabejacite, Soddyite, Tyuyamunite, Uranopilite, Zippeite, Pseudojohannite, Sejkoraite-(Y) | 236802 | Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic | Červená vein | Plasil et al. (2014) | 10.3190/jgeosci.171 | JG59_223 | Age of recent supergene mineralization. The alteration association of the recent origin, resulting from the weathering and decomposition of the primary uranium minerals, occurring together with copper sulfides, in the old mining workings. | ||||||||||
| Michelle_542 | 65 | 1.8 | Tertiary | Age of basalt dyke | 236802 | Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic | Červená vein | Plasil et al. (2014) | 10.3190/jgeosci.171 | JG59_223 | Age of basalt dyke | ||||||||||
| Michelle_543 | 370 | 290 | Variscan | Age of primary ore mineralization | Chalcopyrite, Uraninite | 236802 | Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic | Červená vein | Plasil et al. (2014) | 10.3190/jgeosci.171 | JG59_223 | Age of primary ore mineralization (from mesothermal fluids) | |||||||||
| Michelle_544 | 543 | 443 | Cambrian-Ordovician | Age of host formation | 236802 | Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic | Červená vein | Plasil et al. (2014) | 10.3190/jgeosci.171 | JG59_223 | Age of host formation | ||||||||||
| Kristen002438 | 270 | 260 | Late Variscan | vein mineralization | Yes | U | 18657 | Slavkovice, Nové Město Na Moravě, Žďár Nad Sázavou District, Vysočina Region, Czech Republic | Vein Deposits of Bohemian Massif | Surán and Veselý (2001) | IAEA-TECDOC_1258 | ||||||||||
| Kristen002439 | 200 | 170 | Kimerian | vein mineralization | Yes | U | 18657 | Slavkovice, Nové Město Na Moravě, Žďár Nad Sázavou District, Vysočina Region, Czech Republic | Vein Deposits of Bohemian Massif | Surán and Veselý (2001) | IAEA-TECDOC_1258 | ||||||||||
| Kristen002440 | 170 | 130 | Kimerian | vein mineralization | Yes | U | 18657 | Slavkovice, Nové Město Na Moravě, Žďár Nad Sázavou District, Vysočina Region, Czech Republic | Vein Deposits of Bohemian Massif | Surán and Veselý (2001) | IAEA-TECDOC_1258 |
| Sample | Source Locality | Reference URL |
|---|---|---|
All locality data graciously provided by mindat.org
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