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

Figure 5

Field view and line drawing of exposed section in the John Hault quarry where sandstone, silty shale, mudrock, and uncharacterized reddish brown material are observable. Folded and normal faulted mudrock beds occur.