Neotectonic markers in the Panafrican belt formations of Cameroon: elements of interpretation and their environmental impacts
Kouankap, Nono Gus D.
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
Kouankap, Nono Gus D., 2006: Neotectonic markers in the Panafrican belt formations of Cameroon: elements of interpretation and their environmental impacts. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 115 - 116., , DOI: 10.23689/fidgeo-1837.
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The North equatorial Panafrican Belt,
whose Cameroonian formations are
dated between 650 and 400 million
years, and which are located in the
North of the Congo Craton, is subdivided
in to three major geodynamic domains:
a north Cameroon domain, a
central Cameroon domain and a south
Cameroon domain. These major domains
are generally, particularly the
central domain, affected by great strikeslip
faults in which the most important
are the central cameroonian shear zone
and the Sanaga fault.
Studies that establish the order of occurrence
of geological events, generally
performed in these domains and particularly
at Banefo area (West Cameroon)
reveal markers of recent tectonics (post
panafrican) that affect the granitogneissic
basement...