Geochemical evolution of micas and Sn-, Nb-, Ta- mineralization associated with the rare metal pegmatite in Angwan Doka, central Nigeria

Author:

Akoh Juliet U.,Ogunleye Paul O.,Ibrahim Aliyu A.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference51 articles.

1. The Togo-Benin-Nigeria shield: evidence of crustal aggregation in the Pan-African belt;Ajibade;Tectonophysics,1989

2. Mineralization controls and petrogenesis of the rare metal pegmatites of Nasarawa area, Central Nigeria;Akintola;Earth Sci. Res. J.,2008

3. Geology and Geochemistry of the Granitoids of Kokoona Area, in Relation to Mineralization, Central Nigeria;Akoh,2014

4. Mineralogical and geochemical evolution of muscovite in the pegmatite group of the Angwan Doka area, Kokoona district: a clue to petrogenesis and tourmaline mineralization potential;Akoh;J. Geochem. Explor.,2014

5. A geological, geochemical and textural study of a LCT pegmatite: implications for the magmatic versus metasomatic origin of Nb–Ta mineralization in the Moose II pegmatite, Northwest Territories, Canada;Anderson;J. Geosci.,2013

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