Locality type: | Deposit |
Classification |
---|
|
Species: | Dickite |
Formula: | Al2(Si2O5)(OH)4 |
Confirmation |
---|
|
Validity: | Believed Valid |
Data |
---|
|
Mineral Data: | Click here to view Dickite data |
Locality Data: | Click here to view Quema deposit, Los Santos Province, Panama |
Data Identifiers |
---|
|
Mindat Occurrence Record ID: | 691964 |
Long-form Identifier: | 1:3:691964:1 |
GUID (UUID V4): | 272c3a40-a1d6-4656-b697-cfbb5f37534e |
Nearest other occurrences of Dickite |
---|
|
|
8.1km (5.1 miles) | ⓘLa Pava deposit, Los Santos Province, Panama |
References |
---|
|
Corral, I., Griera, A., Gras, D. M. G., Corbella, M., i Sabaté, À. C., Piineda-Falconett, M., & i López, E. C. (2011). Geology of the Cerro Quema Au-Cu deposit (Azuero Peninsula, Panama). Geologica acta: an international earth science journal, 9(3), 481-498. Corral, I., Cardellach, E., Corbella, M., Canals, À., Gómez-Gras, D., Griera, A., & Cosca, M. A. (2016). Cerro Quema (Azuero Peninsula, Panama): Geology, Alteration, Mineralization, and Geochronology of a Volcanic Dome-Hosted High-Sulfidation Au-Cu Deposit. Economic Geology, 111(2), 287-310. |
Reference Search (possible matching items) |
---|
| Corral, Isaac, Cardellach, Esteve, Corbella, Mercè, Canals, Àngels, Gómez-Gras, David, Griera, Albert, Cosca, Michael A. (2016) Cerro Quema (Azuero Peninsula, Panama): Geology, Alteration, Mineralization, and Geochronology of a Volcanic Dome-Hosted High-Sulfidation Au-Cu Deposit. Economic Geology, 111 (2) 287-310 doi:10.2113/econgeo.111.2.287 | Journal (article/letter/editorial) | Vol. 111 March–April No. 2 Cerro Quema (Azuero Peninsula, Panama): Geology, Alteration, Mineralization...a Volcanic Dome-Hosted High-Sulfidation Au-Cu Deposit Isaac Corral,1,2,† Esteve Cardellach,1 Mercè Corbella...Cerro Quema (Azuero Peninsula, southwest Panama) is a high-sulfidation epithermal Au-Cu deposit hosted...hosted by a dacite dome complex of the Río Quema Formation (late Campanian to Maastrichtian), a fore-arc basin...age of lower Eocene (~55–49 Ma) for the Cerro Quema deposit. It was probably triggered by the emplacement |
|