Progradation along a deeply submerged Oligocene-Miocene heterozoan carbonate shelf: How sensitive are clinoforms to sea level variations?

摘要

We combine two- and three-dimensional seismic stratigraphic interpretation with paleobathymetric analysis from benthic foraminifera to understand the genetic significance of prominent seismic discontinuity surfaces typically mapped as sequence boundaries and flooding surfaces in the late Paleogene–early Neogene northern Carnarvon Basin.