Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Oluseyi Adunola Bamisaiye"'
Autor:
Babatunde Joseph Fagbohun, Ayotunde Allen Omitogun, Femi Joshua Ayoola, Oluseyi Adunola Bamisaiye
Publikováno v:
Geology, Ecology, and Landscapes, Pp 1-19 (2024)
The Zuru Schist Belt in Northwest Nigeria is one of the auriferous schist belts occurring in the western half of Nigeria. The gold mineralization largely hosted within Neoproterozoic metasedimentary rocks is considered orogenic. In an attempt to unde
Externí odkaz:
https://doaj.org/article/a17b3fd69430470fa838e687b9d1562e
Autor:
Ola Peter Sunday1 (AUTHOR) psola@futa.edu.ng, Oluseyi Adunola, Bamisaiye1 (AUTHOR), Thaddeus, Idowu2 (AUTHOR)
Publikováno v:
Lithology & Mineral Resources. Nov2020, Vol. 55 Issue 6, p528-537. 10p.
Autor:
Babatunde Joseph Fagbohun, Ayotunde Allen Omitogun, Oluseyi Adunola Bamisaiye, Femi J. Ayoola
Publikováno v:
Geocarto International. 37:978-998
Mapping of the major structures in the Zuru schist belt and preliminary evaluation of distribution of the locations of gold mineralization relative to these structures was achieved using remote sen...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f35eada1aa27837d0fd3532ceeae5dfb
https://doi.org/10.1080/10106049.2020.1753822
https://doi.org/10.1080/10106049.2020.1753822
Publikováno v:
Heliyon, Vol 7, Iss 6, Pp e07174-(2021)
Heliyon
Heliyon
The Okemesi area, southwestern Nigeria, is part of the Ilesha schist belt and play host to the Okemesi fold belt and the Ifewara Shear Zone. Nappe structures had been proposed for some parts of Southwestern Nigeria without very clear meso or micro st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::83976dd745a0e17cc27b918935bfcc01
http://www.sciencedirect.com/science/article/pii/S2405844021012779
http://www.sciencedirect.com/science/article/pii/S2405844021012779
Autor:
Oluseyi Adunola Bamisaiye, Blessing Adeoti, Femi J. Ayoola, Babatunde Joseph Fagbohun, Ayotunde Allen Omitogun
Publikováno v:
Arabian Journal of Geosciences. 14
The Zuru Schist Belt is one of the gold-bearing schist belts in northwestern Nigeria. The gold mineralisation is mainly associated with NE-trending shear zones and is hosted in veins of quartz, quartz-tourmaline and quartz-feldspar. In this study, th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c0fd833e013fb91a786a21cff642dbd
https://doi.org/10.1007/s12517-021-06828-7
https://doi.org/10.1007/s12517-021-06828-7
Akademický článek
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Autor:
Babatunde Joseph Fagbohun, Femi J. Ayoola, Oluseyi Adunola Bamisaiye, Ayotunde Allen Omitogun
Publikováno v:
Ore Geology Reviews. 116:103260
The Trans-Sahara belt is one of the mobile belts formed during the Pan African orogeny that spans between ~870 and ~550 Ma. The Trans-Sahara belt was formed as result of the collision between the converging West African craton, Congo craton, and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff33bfc9a59343cefac7fe93d9c555b5
https://doi.org/10.1016/j.oregeorev.2019.103260
https://doi.org/10.1016/j.oregeorev.2019.103260