|
|
Seismic Stratigraphy
IntroductionSeismic stratigraphic analysis of the seismic reflection data identified three main units: Cretaceous and Tertiary continental shelf strata, deposits of unknown age that fill an extensive system of ancient paleochannels, and modern (Pleistocene and younger) surficial sediment accumulations. A regionally defined transgressive unconformity separates lithified underlying continental shelf strata and paleochannel fill, from overlying unconsolidated marine sediment. Paleochannels are present both above and below this unconformity, indicating that the ages and origins of the incisions and fill vary significantly.
|