Soft-Sediment Deformation Structures Interpreted as Seismites in the Kolankaya Formation, Denizli Basin (SW Turkey)

Figure 5

Clastic dikes in the study area. (a) Gravelly coarse-grained sand cuts through the sand layer and is intruded into overlying marls (37.769 N, 29.155 E). (b) Clastic material with fragments up to a max. 4 cm of gravel size intruded through marls (27.792 N, 29.130 E).