Karst sub-basins and their relationship to the transport of Tertiary siliciclastic sediments on the Florida Platform - Perspectives in Carbonate Geology - page 186

E' Southeast E'

North

km

F' North South F'

km

F' North South F'

km

G' North

South G'

km

Fig. 9. Interpreted cross-sections from seismic data collected in Charlotte Harbor - see Fig. 7 for location. Cross-sections
reveal signifi cant deformation in the form of warps, sags and folds. Also shown are prograding clinoforms, numerous,
small palaeofl uvial cut-and-fi ll structures and small, buried sinkholes. Separate seismic sequences are identifi ed as A-F.

Fig. 10. Detail of fold in seismic
data from southern Charlotte Harbor.
This fold or warp reveals high-angle
faulting indicating lithifi cation prior to
deformation. This structure is a dome-
like fold exhibiting limited lateral
extent and a non anticlinal three-
dimensional geometry. See Fig. 8 for
location.