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. |
Acanthite | Allophane | Aragonite | Baryte | Calcite | Clay | Malachite | None | Not in a structural group | Oxalate |
Rocksalt | Smectite-vermiculite |
Acanthite (*) | Anglesite (*) | Azurite (*) | Bromargyrite (*) | Calcite (*) |
Cerussite (*) | Chrysocolla (*) | Malachite (*) | Montmorillonite (*) | Smithsonite (*) |
Whewellite (*) |
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 |
---|---|---|---|---|---|---|---|
Acanthite (*) | Acanthite | Ag2S | 299 | 0 | 1 | 270455 | 2793 |
Anglesite (*) | Baryte | Pb(SO4) | 299 | 0 | 1 | 270455 | 2734 |
Azurite (*) | Not in a structural group | Cu3(CO3)2(OH)2 | 299 | 0 | 1 | 270455 | 5509 |
Bromargyrite (*) | Rocksalt | AgBr | 299 | 0 | 1 | 270455 | 227 |
Calcite (*) | Calcite | Ca(CO3) | 299 | 0 | 1 | 270455 | 27770 |
Cerussite (*) | Aragonite | Pb(CO3) | 299 | 0 | 1 | 270455 | 4979 |
Chrysocolla (*) | Allophane | (Cu2-xAlx)H2-xSi2O5(OH)4·nH2O | 299 | 0 | 1 | 270455 | 3531 |
Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 299 | 0 | 1 | 270455 | 12537 |
Montmorillonite (*) | Clay Smectite-vermiculite | (Na,Ca)0.3(Al,Mg)2Si4O10(OH)2·nH2O | 299 | 0 | 1 | 270455 | 1508 |
Smithsonite (*) | Calcite | Zn(CO3) | 299 | 0 | 1 | 270455 | 2473 |
Whewellite (*) | Oxalate | Ca(C2O4)·H2O | 299 | 0 | 1 | 270455 | 66 |
Age ID | Locality Notes |
---|---|
Michelle_804 | Powwow Member of the Hueco Limestone |
Michelle_805 | Supergene silver-bearing ores are found principally along small fractures or near surface faults that generally are conformable with the bedding. The ores probably formed at low temperatures during Basin and Range extension |
Michelle_806 | Tertiary igneous rocks of the region |
Michelle_847 | Laramide folding and thrusting/deformation was responsible for the intial tilting of the Permian through the Cretaceous strat prior to basin and range modification. |
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_804 | 299 | 252 | Permian | Age of host rock | Yes | 31002 | Plata Verde Mine, Van Horn Mts, Hudspeth Co., Texas, USA | Plata Verde Mine | Price (1982) | BEGMRC70_1 | Age of the Powwow Member of the Hueco Limestone. Host rock of the Plata Verde Mine. | ||||||||||
Michelle_805 | 27 | 0 | 27-23 to Recent | Age of supergene mineralization | Yes | 31002 | Plata Verde Mine, Van Horn Mts, Hudspeth Co., Texas, USA | Plata Verde Mine | Price (1982) | BEGMRC70_1 | Age of basin and range extension that is responsible for the supergene mineralization | ||||||||||
Michelle_806 | 65 | 2.6 | Tertiary | Age of igneous activity | Yes | 31002 | Plata Verde Mine, Van Horn Mts, Hudspeth Co., Texas, USA | Plata Verde Mine | Price (1982) | BEGMRC70_1 | Age of tertiary igenous activity in the region | ||||||||||
Michelle_847 | 100 | 23 | Late Cretaceous to Early Tertiary | Age of Laramide deformation | Yes | 31002 | Plata Verde Mine, Van Horn Mts, Hudspeth Co., Texas, USA | Plata Verde Mine | Price (1982) | BEGMRC70_1 | Age of Laramide deformation |
Sample | Source Locality | Reference URL |
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