Genesis of Clastic Dykes and Soft-Sediment Deformation Structures in the Mamfe Basin, South-West Region, Cameroon: Field Geology Approach

Figure 4

Photograph of a clastic dyke at Egbekaw cross cutting a silty shale bed showing (a) a normal dextral fault, (b) normal sinistral fault with fault plane filled by clastic dykes.

(a)

(b)