| 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. |
| Biphosphammite | Gypsum | None | Quartz | Rocksalt |
| Biphosphammite (*) | Guanine (*) | Gypsum (*) | Halite (*) | 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 |
|---|---|---|---|---|---|---|---|
| Biphosphammite (*) | Biphosphammite | (NH4)H2(PO4) | 0 | 0 | 0 | 11 | |
| Guanine (*) | None | C5H3(NH2)N4O | 0 | 0 | 0 | 7 | |
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 0 | 0 | 0 | 6890 | |
| Halite (*) | Rocksalt | NaCl | 0 | 0 | 0 | 1398 | |
| Quartz (*) | Quartz | SiO2 | 0 | 0 | 0 | 61156 |
| Age ID | Locality Notes |
|---|---|
| Michelle_0022 | Cave in formation |
| 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_0022 | 0 | 0 | 0 | Age of mineralization | Biphosphammite, Guanine, Gypsum, Halite | 250080 | Cueva Lechuza De Campanario, Cordillera De La Sal, San Pedro De Atacama, El Loa Province, Antofagasta, Chile | Cueva Lechuza de Campanario | De Waele et al. (2009) | G2_113 | Mineralization occurs within caves in the Oligocene-Miocene aged Cordillera de la Sal evaporites. |
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