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

<table>Clastic dikes that are seen in the study area. (a) In this figure coarse-grained sand clearly intrudes overlying layered marls (37.768 N, 29.152 E). (b) Sills and dikes of fine-grained sand in marls (37.768 N, 29.154 E).</table>

The Scientific World Journal

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Figure 4

Figure 4: Soft-Sediment Deformation Structures Interpreted as Seismites in the Kolankaya Formation, Denizli Basin (SW Turkey) 