Abstract
This paper examines the relationship between earthquake epicentres and the existence of fossil plate boundaries in West Africa. Several suture zones in the region have been identified and mapped using geological and geophysical methods, and many of them appear parallel to, or correlate with, recognizable paleo-rift and paleo-compressional zones within and adjacent to the West African craton. Plate interaction between the craton and adjacent landmasses in the Precambrian resulted in the production of a continental block made up of a mosaic of units whose boundaries are marked by suture zones, along which the epicentres of historical and recent earthquakes appear to cluster.
The indications are that the distribution of earthquakes and suture zones in space and time could be the best available index to the location of future damaging earthquakes. Data currently available are insufficient to estimate the average recurrence rate of significant earthquakes or the magnitude of the largest possible earthquake. However, the close association between fossil plate boundaries/suture zones and earthquakes in this region indicates the importance of mapping sutures and faults/paleo-rifts as a major initial step in the study of the seismic hazard of intraplate regions.
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© 1992 Friedr. Vieweg & Sohn Verlagsgesellschaft mbH, Braunschweig/Wiesbaden
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Onuoha, K.M., Ezeh, C.C. (1992). Fossil plate boundaries in West Africa and their bearing on seismotectonics. In: Freeth, S.J., Ofoegbu, C.O., Onuoha, K.M. (eds) Natural Hazards in West and Central Africa. International Monograph Series. Vieweg+Teubner Verlag, Wiesbaden. https://doi.org/10.1007/978-3-663-05239-5_3
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DOI: https://doi.org/10.1007/978-3-663-05239-5_3
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