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Jbel Merguechoum fluorite–barite deposit, Taourirt Province, Oriental Region, Moroccoi
| Regional Level Types | |
|---|---|
| Jbel Merguechoum fluorite–barite deposit | Deposit |
| Taourirt Province | Province |
| Oriental Region | Region |
| Morocco | Country |
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Latitude & Longitude (WGS84):
34° 20' 23'' North , 2° 48' 3'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
A granite-hosted fluorite–barite vein-type deposit whose trace and rare-earth element (REE) geochemistry, role of structural defects and trace elements in fluorite coloration, and specimen quality of the fluorite in relation to geoheritage. The Paleozoic basement of the Eastern Meseta, which includes metamorphosed sedimentary and volcanic-sedimentary units, is exposed in several inliers, such as Jbel Merguechoum. Mesozoic sedimentary layers unconformably overlie these outcrops. Within the Jbel Merguechoum inlier, the fluorite–barite ore is hosted by a Neovariscan granite, described as a coarse-grained, leucocratic, porphyritic granite.
Stage I (Primary hydrothermal—Early hydrothermal stage). This stage is defined by massive to metasomatic texture resulting from direct replacement of Neovariscan granite.
Stage II (Coarse-crystalline hydrothermal—late hydrothermal stage). This stage is defined by large, well-formed crystals exceeding 1 cm in size, crystallized in open cavities. Diagnostic criteria include crystal size ≥ 1 cm and the absence of metasomatic replacement textures. The mineral assemblage comprises large, well-formed crystals of fluorite, barite, quartz, and pyrite.
Stage III (Supergene (oxidation/weathering)—post-ore stage). This stage is defined by near-surface alteration of earlier hypogene minerals. Diagnostic criteria include occurrence as crusts, coatings, or veins that physically crosscut Stages I and II.
Stage I (Primary hydrothermal—Early hydrothermal stage). This stage is defined by massive to metasomatic texture resulting from direct replacement of Neovariscan granite.
Stage II (Coarse-crystalline hydrothermal—late hydrothermal stage). This stage is defined by large, well-formed crystals exceeding 1 cm in size, crystallized in open cavities. Diagnostic criteria include crystal size ≥ 1 cm and the absence of metasomatic replacement textures. The mineral assemblage comprises large, well-formed crystals of fluorite, barite, quartz, and pyrite.
Stage III (Supergene (oxidation/weathering)—post-ore stage). This stage is defined by near-surface alteration of earlier hypogene minerals. Diagnostic criteria include occurrence as crusts, coatings, or veins that physically crosscut Stages I and II.
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
9 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 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 3 - Halides | |||
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| Unclassified | |||
| ⓘ | 'Alkali Feldspar' | - | |
| ⓘ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| F | ⓘ Fluorite | CaF2 |
| Na | Sodium | |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| S | Sulfur | |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Fluorite | CaF2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
Other Regions, Features and Areas containing this locality
AfricaContinent
African PlateTectonic Plate
- Atlas basinBasin
- Atlas MountainsMountain Range
Northwest Africa MeteoritesGroup of Meteorite Fall Locations
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References
[1]Cherai, Mohammed; Benamrane, Mohammed; Rddad, Larbi; Németh, Károly (2026) Granite-Hosted Fluorite–Barite Veins at Jbel Merguechoum (Northeastern Morocco): Paragenesis, Trace-Elements and REE Geochemistry, and Constraints on the Origin of Green and Purple Coloration. Geosciences, 16 (10). p.403. doi:10.3390/geosciences16100403