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. |
Corundum | Feldspar | Lepidocrocite | None | Quartz |
Hematite (*) | Lepidocrocite (*) | Orthoclase (*) | Quartz (*) |
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 |
---|---|---|---|---|---|---|---|
Hematite (*) | Corundum | Fe2O3 | 3.36 | 3.24 | 1 | 113449 | 14640 |
Lepidocrocite (*) | Lepidocrocite | Fe3+O(OH) | 3.36 | 3.24 | 1 | 113449 | 581 |
Orthoclase (*) | Feldspar | K(AlSi3O8) | 3.36 | 3.24 | 0 | 2349 | |
Quartz (*) | Quartz | SiO2 | 3.36 | 3.24 | 1 | 113449 | 61156 |
Age ID | Locality Notes |
---|---|
Michelle_507 | Baylissite occurs as a recent secondary mineral in alpine fissures of the Gerstenegg-Sommerloch tunnel in the Grimsel Pass area of the Aar Massif. Pliocene hydrothermal breccia mineralization in the Grimsel area demonstrates that meteoric waters penetrated deep into the Aar massif. The tunnels are utilized by utility companies. |
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_507 | 3.36 | 3.24 | 3.30±0.06 | Ar-Ar | Age of hydrothermal alteration | adularia | 22954 | Grimsel Pass, Grimsel Area, Hasli Valley, Bern, Switzerland | Grimsel Pass | Hofmann et al. (2004) | SMPM84_271 | Age of hydrothermal alteration. |
Sample | Source Locality | Reference URL |
---|---|---|
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