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. |
Beryl | None | Quartz | Tourmaline |
Cordierite (*) | Pigotite (*) | Quartz (*) | Schorl (*) |
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 |
---|---|---|---|---|---|---|---|
Cordierite (*) | Beryl | Mg2Al4Si5O18 | 0 | 0 | 1 | 118907 | 1008 |
Pigotite (*) | None | Al4C6H5O10·13H2O (?) | 0 | 0 | 1 | 118910 | 3 |
Quartz (*) | Quartz | SiO2 | 0 | 0 | 1 | 118908 | 61156 |
Schorl (*) | Tourmaline | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 0 | 0 | 1 | 118911 | 2705 |
Age ID | Locality Notes |
---|---|
Michelle_751 | Near Porthcurno and Porthchapel, St. Levan. Pigotite occurs as a biomineral in granitic caves/fissures as a result of organic acids from seeping vegetation combined with aluminum derived from feldspar. |
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_751 | 0 | 0 | Recent | Age of pigotite | high | Pigotite | 1389 | Cripp's Cove, Treen, St Levan, Cornwall, England, UK | Cripp's Cove | Creighton (1894) | GM1_223 | Pigotite occurs as a biomineral in granitic caves/fissures as a result of organic acids from seeping vegetation combined with aluminum derived from feldspar. |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
All age data...
Other copyright data...