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Cerro Kiosko deposit, Bayaguana District, Monte Plata Province, Dominican Republici
| Regional Level Types | |
|---|---|
| Cerro Kiosko deposit | Deposit |
| Bayaguana District | District |
| Monte Plata Province | Province |
| Dominican Republic | Country |
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Latitude & Longitude (WGS84):
18° 49' 20'' North , 69° 39' 32'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Bayaguana | 21,055 (2016) | 8.4km |
| Monte Plata | 15,532 (2016) | 13.2km |
| Gonzalo | 2,027 (2016) | 17.3km |
| Sabana Grande de Boyá | 16,834 (2016) | 19.6km |
| El Puerto | 3,278 (2016) | 20.7km |
The Cerro Kiosko deposit consists of a 1.25-to 22-m-thick, ~1,100-m-long, and ~400-m-deep tabular quartz-sulfide vein swarm hosted by silicic-altered basaltic andesites and andesites of the upper unit, and also includes sulfide disseminations. The vein swarm is composed of stringers and massive sulfide lodes largely controlled by NW-striking normal faults that dip ~60° to the southwest. Reserves: 2.8 Mt at 2.2 g/t Au, 4.7 g/t Ag, 0.6% Cu
At Cerro Kiosko, an outer extensive domain of moderate-intensity propylitic alteration grades inward and downward to narrower domains of phyllic and intermediate argillic alteration. Propylitic alteration caused chlorite to replace clinopyroxenes and the glassy matrix, and produced thin veinlets of chlorite and albite alteration of plagioclase. Phyllic alteration caused fine-grained muscovite to replace plagioclase and parts of the groundmass. In intermediate argillic zones, fine-grained quartz and kaolinite pervasively altered the volcanic rocks so that no original textural features are recognizable. Fine-grained pyrite dissemination increased markedly (>50% modal) along with the degree of silicic and kaolinite alteration.
Cu (± Ag ± Au) mineralization produced 0.5-to ~30-cm-thick massive sulfide stage 1 veins and lodes within strongly quartz altered host rocks. The thickest veins have multiple internal growth bands. Stage 1 caused hydrofracturing of the previously altered host rocks and cementation of the fragments by pyrite. Although not common, quartz fragments are locally cemented by fahlore. A transitional shallow porphyry–deep high-sulfidation epithermal environment for the deposition of ores.
At Cerro Kiosko, an outer extensive domain of moderate-intensity propylitic alteration grades inward and downward to narrower domains of phyllic and intermediate argillic alteration. Propylitic alteration caused chlorite to replace clinopyroxenes and the glassy matrix, and produced thin veinlets of chlorite and albite alteration of plagioclase. Phyllic alteration caused fine-grained muscovite to replace plagioclase and parts of the groundmass. In intermediate argillic zones, fine-grained quartz and kaolinite pervasively altered the volcanic rocks so that no original textural features are recognizable. Fine-grained pyrite dissemination increased markedly (>50% modal) along with the degree of silicic and kaolinite alteration.
Cu (± Ag ± Au) mineralization produced 0.5-to ~30-cm-thick massive sulfide stage 1 veins and lodes within strongly quartz altered host rocks. The thickest veins have multiple internal growth bands. Stage 1 caused hydrofracturing of the previously altered host rocks and cementation of the fragments by pyrite. Although not common, quartz fragments are locally cemented by fahlore. A transitional shallow porphyry–deep high-sulfidation epithermal environment for the deposition of ores.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
15 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Idaite | 2.CB.15a | Cu5FeS6 |
| ⓘ | Altaite | 2.CD.10 | PbTe |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Calaverite | 2.EA.10 | AuTe2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Goldfieldite | 2.GB.05 | (Cu4◻2)(Cu4Cu+2)Te4S12S |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | Enargite | 2.KA.05 | Cu3AsS4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Group 9 - Silicates | |||
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Tetrahedrite Group' | - | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| S | Sulfur | |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Enargite | Cu3AsS4 |
| S | ⓘ Galena | PbS |
| S | ⓘ Goldfieldite | (Cu4◻2)(Cu4Cu2+)Te4S12S |
| S | ⓘ Idaite | Cu5FeS6 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Tetrahedrite Group | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Fe | Iron | |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Idaite | Cu5FeS6 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Enargite | Cu3AsS4 |
| Cu | ⓘ Goldfieldite | (Cu4◻2)(Cu4Cu2+)Te4S12S |
| Cu | ⓘ Idaite | Cu5FeS6 |
| Cu | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| As | Arsenic | |
| As | ⓘ Enargite | Cu3AsS4 |
| As | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Te | Tellurium | |
| Te | ⓘ Altaite | PbTe |
| Te | ⓘ Calaverite | AuTe2 |
| Te | ⓘ Goldfieldite | (Cu4◻2)(Cu4Cu2+)Te4S12S |
| Au | Gold | |
| Au | ⓘ Calaverite | AuTe2 |
| Au | ⓘ Native Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Altaite | PbTe |
| Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
Caribbean PlateTectonic Plate
North America
- Central AmericaSubregion
North America Plate
- Greater Antilles ArcVolcanic Arc
The CaribbeanRegion
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References
[1]Torró, Lisard, Camprubí, Antoni, Proenza, Joaquín A., León, Paulo, Stein, Holly J., Lewis, John F., Nelson, Carl E., Chavez, Cevero, Melgarejo, Joan Carles (2017) Re-Os and U-Pb Geochronology of the Doña Amanda and Cerro Kiosko Deposits, Bayaguana District, Dominican Republic: Looking Down for the Porphyry Cu-Mo Roots of the Pueblo Viejo-Type Mineralization in the Island-Arc Tholeiitic Series of the Caribbean. Economic Geology, 112 (4) 829-853 doi:10.2113/econgeo.112.4.829
Nelson, Carl E., Polanco, José, Macassi, Arturo, Domínguez, Hugo, Proenza, Joaquín A., Torró, Lisard, Rhys, David, Iturralde-Vinent, Manuel (2020) The Hatillo Limestone, Pueblo Viejo district, Dominican Republic: Marginal reef or impermeable cap?. Boletín de la Sociedad Geológica Mexicana, 72 (3) doi:10.18268/bsgm2020v72n3a011119