Panj-Kuh iron deposit (Panj-Kuh iron mine), Damghan County, Semnan Province, Irani
| Regional Level Types | |
|---|---|
| Panj-Kuh iron deposit (Panj-Kuh iron mine) | Deposit |
| Damghan County | County |
| Semnan Province | Province |
| Iran | Country |
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Latitude & Longitude (WGS84):
35° 28' 19'' North , 54° 12' 0'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
The Panj-Kuh iron deposit is located 50 km southeast of Damghan within the Central Iranian Zone (CIZ).
The Panj-Kuh deposit is hosted mainly in the Eocene andesite and basalt volcano-pyroclastic rocks as well as Oligocene syenite, monzonite and gabbro plutonic rocks. The mineralisation of the Panj-Kuh iron deposit occurred in both orthomagmatic and hydrothermal stages. In the orthomagmatic stage, associated with crystallisation of a gabbroic magma, iron mineralisation occurred in the form of disseminated and massive ores. In the second stage, the monzonitic intrusion was injected into the gabbroic, volcano-sedimentary and volcanic rocks and caused hydrothermal iron mineralisation such as skarnisation. Pyroxene, epidote and amphibole are the main silicate minerals; magnetite and less hematite are the principal ore mineral, pyrite, chalcopyrite, marcasite, galena, sphalerite, chalcocite, and covellite are minor ore constituents (Sheibi, 2014; Nabatian et al., 2015; Sheibi et al., 2016).
The Panj-Kuh Fe oxide deposit is estimated to contain 100 million tons of iron ore with an average Fe2O3 = 84.2%, and FeO = 8.5%. The deposit tends to be zoned vertically from magnetite dominant at depth to hematite-dominantat upper levels. The ore body occurs within volcanic rocks that were brecciated during fault movement along bounding shear zones. Mineralisation occurs dominantly as disseminations, veins, and breccia infill.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
25 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:
| ⓘ Actinolite Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Albite Formula: Na(AlSi3O8) Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 Reference: Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241. |
| ⓘ Analcime Formula: Na(AlSi2O6) · H2O Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Azurite Formula: Cu3(CO3)2(OH)2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241. |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Calcite Formula: CaCO3 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Chalcocite Formula: Cu2S Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Chalcopyrite Formula: CuFeS2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ 'Chlorite Group' Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ 'Clinopyroxene Subgroup' Description: Diopside-hedenbergite series (Sheibi, 2014) Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Covellite Formula: CuS Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Diopside Formula: CaMgSi2O6 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102. |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241. |
| ⓘ Ferro-actinolite Formula: ◻Ca2Fe2+5(Si8O22)OH2 Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Fluorapatite Formula: Ca5(PO4)3F Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Galena Formula: PbS Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Hematite Formula: Fe2O3 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Ilmenite Formula: Fe2+TiO3 Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ 'K Feldspar' Formula: KAlSi3O8 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241. |
| ⓘ Marcasite Formula: FeS2 Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Marialite Formula: Na4Al3Si9O24Cl Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Pyrite Formula: FeS2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., and Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 211-241; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Quartz Formula: SiO2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Rutile Formula: TiO2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102. |
| ⓘ Sphalerite Formula: ZnS Reference: Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Titanite Formula: CaTi(SiO4)O Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102; Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628. |
| ⓘ Tremolite Formula: ◻Ca2Mg5(Si8O22)(OH)2 Reference: Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
| Group 9 - Silicates | |||
| ⓘ | Actinolite | 9.DE.10 | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| ⓘ | Analcime | 9.GB.05 | Na(AlSi2O6) · H2O |
| ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Ferro-actinolite | 9.DE.10 | ◻Ca2Fe2+5(Si8O22)OH2 |
| ⓘ | Marialite | 9.FB.15 | Na4Al3Si9O24Cl |
| ⓘ | Titanite | 9.AG.15 | CaTi(SiO4)O |
| ⓘ | Tremolite | 9.DE.10 | ◻Ca2Mg5(Si8O22)(OH)2 |
| Unclassified Minerals, Rocks, etc. | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'K Feldspar' | - | KAlSi3O8 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| H | ⓘ Ferro-actinolite | ◻Ca2Fe52+(Si8O22)OH2 |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| H | ⓘ Analcime | Na(AlSi2O6) · H2O |
| H | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| C | Carbon | |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Ferro-actinolite | ◻Ca2Fe52+(Si8O22)OH2 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| O | ⓘ Titanite | CaTi(SiO4)O |
| O | ⓘ K Feldspar | KAlSi3O8 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Analcime | Na(AlSi2O6) · H2O |
| O | ⓘ Marialite | Na4Al3Si9O24Cl |
| O | ⓘ Fluorapatite | Ca5(PO4)3F |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Diopside | CaMgSi2O6 |
| O | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| F | Fluorine | |
| F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| F | ⓘ Fluorapatite | Ca5(PO4)3F |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Na | ⓘ Marialite | Na4Al3Si9O24Cl |
| Mg | Magnesium | |
| Mg | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Mg | ⓘ Diopside | CaMgSi2O6 |
| Mg | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Al | ⓘ K Feldspar | KAlSi3O8 |
| Al | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Al | ⓘ Marialite | Na4Al3Si9O24Cl |
| Si | Silicon | |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Ferro-actinolite | ◻Ca2Fe52+(Si8O22)OH2 |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Si | ⓘ Titanite | CaTi(SiO4)O |
| Si | ⓘ K Feldspar | KAlSi3O8 |
| Si | ⓘ Analcime | Na(AlSi2O6) · H2O |
| Si | ⓘ Marialite | Na4Al3Si9O24Cl |
| Si | ⓘ Diopside | CaMgSi2O6 |
| Si | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| P | Phosphorus | |
| P | ⓘ Fluorapatite | Ca5(PO4)3F |
| S | Sulfur | |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Galena | PbS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Covellite | CuS |
| Cl | Chlorine | |
| Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Cl | ⓘ Marialite | Na4Al3Si9O24Cl |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| K | ⓘ K Feldspar | KAlSi3O8 |
| Ca | Calcium | |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Ferro-actinolite | ◻Ca2Fe52+(Si8O22)OH2 |
| Ca | ⓘ Titanite | CaTi(SiO4)O |
| Ca | ⓘ Fluorapatite | Ca5(PO4)3F |
| Ca | ⓘ Diopside | CaMgSi2O6 |
| Ca | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Ti | ⓘ Titanite | CaTi(SiO4)O |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Ti | ⓘ Rutile | TiO2 |
| Fe | Iron | |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Ferro-actinolite | ◻Ca2Fe52+(Si8O22)OH2 |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Cu | Copper | |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Covellite | CuS |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)Sheibi, M. (2014) Mineral chemistry and mass changes of elements during alteration of Panj-Kuh intrusive body (Damghan, Iran). Geopersia, 4, 1, 87-102.
Nabatian, G., Rastad, E., Neubauer, F., Honarmand, M., Ghaderi, M. (2015) Fe and Fe-Mn mineralization in Iran: Implication from Tethyan Metallogeny. Australian Journal of Earth Sciences, 62, 2, 211-241.
Sheibi, M., Mirnejad, H., and Pooralizadeh Moghaddam, M. (2016) Magnetic susceptibility anisotropy as a predictive exploration tool of metasomatic iron oxide deposits: Example from the Panj-Kuh iron ore body, NE Iran. Ore Geology Reviews, 72, 1, 612-628.
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Panj-Kuh iron deposit, Damghan County, Semnan Province, Iran