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| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Access Rights | Open Access | ||
| Title | Rare-Element Pegmatites Rocks Rich and Li of the Aïr Massif of the Tchirozerine: Mineralogy and Chemical Composition Agadez Region-Northern Niger | ||
| Journal | Open Journal of Applied Sciences | ||
| Authors | Mama Ntoumbé | Author | |
| Bassara, Hamza | Author | ||
| Adama, Amaya | Author | ||
| Zéphyrin, Awona Paul | Author | ||
| Limbisoa, Nomenjanahary | Author | ||
| Page(s) | 171-181 | ||
| Publisher | Science Research Publishing | ||
| DOI | doi:10.4236/ojapps.2024.141013 | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 18012424 | Long-form Identifier | mindat:1:5:18012424:8 |
| GUID | 0 | ||
| Full Reference | Mama Ntoumbé, Bassara, Hamza, Adama, Amaya, Zéphyrin, Awona Paul, Limbisoa, Nomenjanahary (n.d.) Rare-Element Pegmatites Rocks Rich and Li of the Aïr Massif of the Tchirozerine: Mineralogy and Chemical Composition Agadez Region-Northern Niger. Open Journal of Applied Sciences, 14. 171-181 doi:10.4236/ojapps.2024.141013 | ||
| Plain Text | Mama Ntoumbé, Bassara, Hamza, Adama, Amaya, Zéphyrin, Awona Paul, Limbisoa, Nomenjanahary (n.d.) Rare-Element Pegmatites Rocks Rich and Li of the Aïr Massif of the Tchirozerine: Mineralogy and Chemical Composition Agadez Region-Northern Niger. Open Journal of Applied Sciences, 14. 171-181 doi:10.4236/ojapps.2024.141013 | ||
| In | Link this record to the correct parent record (if possible) | ||
| Abstract/Notes | The lithium potential in the Aïr massif is represented by mineral index of spodumene pegmatites and, lepidolite pegmatites. The mineral deposits of lithium occur in cluster or veins that cut the host rock or are located near the contact between the greenstone belt and granitic massif. The evidence of lithium is in the form of clusters or disseminated and stockwerk. Mineralogical characteristics show similarities between the Air Massif pegmatites and indicate the same homogenous source during the magma-generation process. The pegmatite rocks attracted the attention due to their wide exposure and composition, well appearance, and economically hosting of significant rare earth metals such as Sn and W. The mineralogical and petrographical investigations on the eight pegmatites rocks samples observed have a relative similarity, while a little difference in the shapes attributed to the ratio in the pegmatite rocks of the minerals. The occurrence of the kink band indicates the influence of the tectonic processes which affected the Aïr massif after the emplacement of late magmatic or post-magmatic pegmatites by injection into fractured rocks in the upper part of the crust. The Air Massif pegmatite has higher concentrations Li and of all trace elements except Hf and occasionally Zr, Ti, Sn and Mg of for the economic exploration. | ||
| Locality | Citation Details |
|---|---|
| Aïr Mountains, Agadez, Niger |
| Locality | Mineral(s) |
|---|---|
| Aïr Mountains, Agadez, Niger | ⓘ Albite, ⓘ Biotite, ⓘ Feldspar Group, ⓘ Gneiss, ⓘ Granite, ⓘ Metamorphic rock, ⓘ Microcline, ⓘ Muscovite, ⓘ Oligoclase-Albite, ⓘ Orthoclase, ⓘ Pegmatite, ⓘ Perthite, ⓘ Plagioclase, ⓘ Quartz, ⓘ Rhyolite, ⓘ Spodumene, ⓘ Syenite |
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