The Birimian event in the Baoulé Mossi domain (West African Craton) : regional and global context
The crystalline basement of the West African Craton (WAC) was established during the Siderian to Orosirian (circa 2.35-1.95 Ga) Birimian event through accretion of extensive tracts of juvenile crust that was tectonically juxtaposed with Archean cratons. The Birimian crust is comprised of volcanic be...
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Format: | Other/Unknown Material |
Language: | English |
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Lunds universitet/Geologiska institutionen
2014
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Online Access: | http://lup.lub.lu.se/student-papers/record/4250461 |