Mercedita Cr deposit, Moa-Baracoa District, Holguín Province, Cubai
Regional Level Types | |
---|---|
Mercedita Cr deposit | Deposit |
Moa-Baracoa District | District |
Holguín Province | Province |
Cuba | Country |
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Latitude & Longitude (WGS84):
20° 30' 6'' North , 74° 55' 7'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Moa | 92,852 (2014) | 17.7km |
Río Guayabal de Yateras | 25,753 (2006) | 18.2km |
Sagua de Tánamo | 18,282 (2016) | 34.8km |
Baracoa | 48,362 (2016) | 47.2km |
Guantánamo | 272,801 (2016) | 49.9km |
Mindat Locality ID:
39109
Long-form identifier:
mindat:1:2:39109:3
GUID (UUID V4):
9fc741c3-05c5-4098-b104-862430410157
Largest and most important podiform chromite deposit in America, with calculated reserves exceeding 5 million tons. The largest chromitite body is 600 m long, 250 m wide, and up to 20 m thick. Tabular to lenticular bodies of chromitite of variable size are crosscut by normal faults. The lenses are invariably parallel to the foliation and lineation of host peridotite and are located in the mantle-crust transition zone, characterized by the interlayering of ultramafic and gabbroic rocks. Dunite (from few centimeters to a few meters in thickness) systematically envelopes the chromitite bodies, though chromitite-harzburgite contacts are locally developed. The contact between chromitite and peridotites is generally sharp and only locally gradational.
Located within the World Heritage listed Alejandro de Humbolt National Park.
Coordinates approximate.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
20 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
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Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Antigorite Formula: Mg3(Si2O5)(OH)4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Chalcocite Formula: Cu2S Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Chalcopyrite Formula: CuFeS2 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Chlorite Group' Reference: Acta Geológica Hispánica, 1998, 33(1-4):179-212
Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Chromite Formula: Fe2+Cr3+2O4 Reference: Acta Geológica Hispánica, 1998, 33(1-4):179-212
Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Chromite var. Ferrian Chromite Formula: Fe2+(Cr,Fe3+)2O4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Chrysotile Formula: Mg3(Si2O5)(OH)4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Clinochlore Formula: Mg5Al(AlSi3O10)(OH)8 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Clinopyroxene Subgroup' Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Copper Formula: Cu Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Corundum Formula: Al2O3 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Diopside Formula: CaMgSi2O6 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Enstatite Formula: Mg2Si2O6 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Fayalite-Forsterite Series' Reference: Acta Geológica Hispánica, 1998, 33(1-4):179-212 |
ⓘ Graphite Formula: C Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Hornblende' Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Irarsite Formula: (Ir,Ru,Rh,Pt)AsS Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Laurite Formula: RuS2 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Lizardite Formula: Mg3(Si2O5)(OH)4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Magnetite Formula: Fe2+Fe3+2O4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Millerite Formula: NiS Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Moissanite Formula: SiC Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Olivine Group' Formula: M2SiO4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Pyroxene Group' Formula: ADSi2O6 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Rutile Formula: TiO2 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ 'Serpentine Subgroup' Formula: D3[Si2O5](OH)4 Reference: Acta Geológica Hispánica, 1998, 33(1-4):179-212
Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Spinel Formula: MgAl2O4 Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
ⓘ Zircon Formula: Zr(SiO4) Reference: Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Copper | 1.AA.05 | Cu |
ⓘ | Graphite | 1.CB.05a | C |
ⓘ | Moissanite | 1.DA. | SiC |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Chalcocite | 2.BA.05 | Cu2S |
ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
ⓘ | Irarsite | 2.EB.25 | (Ir,Ru,Rh,Pt)AsS |
ⓘ | Laurite | 2.EB.05a | RuS2 |
ⓘ | Millerite | 2.CC.20 | NiS |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
ⓘ | var. Ferrian Chromite | 4.BB.05 | Fe2+(Cr,Fe3+)2O4 |
ⓘ | Corundum | 4.CB.05 | Al2O3 |
ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
ⓘ | Rutile | 4.DB.05 | TiO2 |
ⓘ | Spinel | 4.BB.05 | MgAl2O4 |
Group 9 - Silicates | |||
ⓘ | Antigorite | 9.ED.15 | Mg3(Si2O5)(OH)4 |
ⓘ | Chrysotile | 9.. | Mg3(Si2O5)(OH)4 |
ⓘ | Clinochlore | 9.EC.55 | Mg5Al(AlSi3O10)(OH)8 |
ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
ⓘ | Enstatite | 9.DA.05 | Mg2Si2O6 |
ⓘ | Lizardite | 9.ED.15 | Mg3(Si2O5)(OH)4 |
ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
Unclassified Minerals, Rocks, etc. | |||
ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
ⓘ | 'Chlorite Group' | - | |
ⓘ | 'Clinopyroxene Subgroup' | - | |
ⓘ | 'Fayalite-Forsterite Series' | - | |
ⓘ | 'Hornblende' | - | |
ⓘ | 'Olivine Group' | - | M2SiO4 |
ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
ⓘ | 'Serpentine Subgroup' | - | D3[Si2O5](OH)4 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
H | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
H | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
H | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
H | ⓘ Lizardite | Mg3(Si2O5)(OH)4 |
C | Carbon | |
C | ⓘ Graphite | C |
C | ⓘ Moissanite | SiC |
O | Oxygen | |
O | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
O | ⓘ Chromite | Fe2+Cr23+O4 |
O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
O | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
O | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
O | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
O | ⓘ Corundum | Al2O3 |
O | ⓘ Diopside | CaMgSi2O6 |
O | ⓘ Enstatite | Mg2Si2O6 |
O | ⓘ Chromite var. Ferrian Chromite | Fe2+(Cr,Fe3+)2O4 |
O | ⓘ Lizardite | Mg3(Si2O5)(OH)4 |
O | ⓘ Magnetite | Fe2+Fe23+O4 |
O | ⓘ Olivine Group | M2SiO4 |
O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
O | ⓘ Pyroxene Group | ADSi2O6 |
O | ⓘ Rutile | TiO2 |
O | ⓘ Spinel | MgAl2O4 |
O | ⓘ Zircon | Zr(SiO4) |
F | Fluorine | |
F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Na | Sodium | |
Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
Mg | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
Mg | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Mg | ⓘ Diopside | CaMgSi2O6 |
Mg | ⓘ Enstatite | Mg2Si2O6 |
Mg | ⓘ Lizardite | Mg3(Si2O5)(OH)4 |
Mg | ⓘ Spinel | MgAl2O4 |
Al | Aluminium | |
Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Al | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Al | ⓘ Corundum | Al2O3 |
Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Al | ⓘ Spinel | MgAl2O4 |
Si | Silicon | |
Si | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Si | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
Si | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
Si | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Si | ⓘ Diopside | CaMgSi2O6 |
Si | ⓘ Enstatite | Mg2Si2O6 |
Si | ⓘ Lizardite | Mg3(Si2O5)(OH)4 |
Si | ⓘ Moissanite | SiC |
Si | ⓘ Olivine Group | M2SiO4 |
Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | ⓘ Pyroxene Group | ADSi2O6 |
Si | ⓘ Zircon | Zr(SiO4) |
S | Sulfur | |
S | ⓘ Chalcocite | Cu2S |
S | ⓘ Chalcopyrite | CuFeS2 |
S | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
S | ⓘ Laurite | RuS2 |
S | ⓘ Millerite | NiS |
Cl | Chlorine | |
Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Ca | Calcium | |
Ca | ⓘ Diopside | CaMgSi2O6 |
Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ti | Titanium | |
Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Ti | ⓘ Rutile | TiO2 |
Cr | Chromium | |
Cr | ⓘ Chromite | Fe2+Cr23+O4 |
Cr | ⓘ Chromite var. Ferrian Chromite | Fe2+(Cr,Fe3+)2O4 |
Fe | Iron | |
Fe | ⓘ Chromite | Fe2+Cr23+O4 |
Fe | ⓘ Chalcopyrite | CuFeS2 |
Fe | ⓘ Chromite var. Ferrian Chromite | Fe2+(Cr,Fe3+)2O4 |
Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
Ni | Nickel | |
Ni | ⓘ Millerite | NiS |
Cu | Copper | |
Cu | ⓘ Copper | Cu |
Cu | ⓘ Chalcocite | Cu2S |
Cu | ⓘ Chalcopyrite | CuFeS2 |
As | Arsenic | |
As | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
Zr | Zirconium | |
Zr | ⓘ Zircon | Zr(SiO4) |
Ru | Ruthenium | |
Ru | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
Ru | ⓘ Laurite | RuS2 |
Rh | Rhodium | |
Rh | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
Ir | Iridium | |
Ir | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
Pt | Platinum | |
Pt | ⓘ Irarsite | (Ir,Ru,Rh,Pt)AsS |
References
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Year (asc) Year (desc) Author (A-Z) Author (Z-A) In-text Citation No.Pujol-Solà, Núria, Joaquín A. Proenza, Antonio Garcia-Casco, José María González-Jiménez, Aleu Andreazini, Joan Carles Melgarejo, and Fernando Gervilla. (2018) "An Alternative Scenario on the Origin of Ultra-High Pressure (UHP) and Super-Reduced (SuR) Minerals in Ophiolitic Chromitites: A Case Study from the Mercedita Deposit (Eastern Cuba)" Minerals 8, no. 10: 433. https://doi.org/10.3390/min8100433
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