Autor: |
E.M. Fozing, M. Kwékam, S. Tetsopgang, T. Njanko, B. Chako-Tchamabé, J. Tcheumenak Kouémo, M. Gountié Dedzo, E.A. Asobo Nkengmatia, C. Njiki Chatué |
Jazyk: |
angličtina |
Rok vydání: |
2021 |
Předmět: |
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Zdroj: |
Solid Earth Sciences, Vol 6, Iss 3, Pp 283-296 (2021) |
Druh dokumentu: |
article |
ISSN: |
2451-912X |
DOI: |
10.1016/j.sesci.2021.06.002 |
Popis: |
The I-type Pan-African Misajé granites, situated in the Western domain of the Central African Fold Belt are among the late-to post tectonic granites that intruded the ante-Pan-African country rocks. In this study, magnetic susceptibility and geochemistry data are integrated to evaluate the productive and non-productive metal potential of these I-type plutonic granites, which comprise Leucocratic granite, Biotite granite, Biotite-hornblende granite, and granodiorites. The magnetic susceptibility of the representative rock samples of the Misajé pluton ranges from 0.001 × 10−3 SI to 33.2 × 10−3 SI. These values indicate the coexistence of both magnetite and ilmenite-series. The magnetite-series (>3 × 10−3 SI; oxidized type) constitute about 32 vol.% while the ilmenite-series ( 1) grains sizes. The Misajé plutonics are high potentially productive in Zn, Th, ilmenite, and magnetite and low productive in Sn, W and Cu though their extension remains limited, probably due to the remobilization of the ancient Paleoproterozoic crust that would have contributed to the dispersing of pre-Pan-African metal deposits. |
Databáze: |
Directory of Open Access Journals |
Externí odkaz: |
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