The first type of barrier island shoreline to be examined in this course is the transgressive type. Transgressive barrier islands can be observed in modern settings to migrate in a landward (up dip) direction as a result of eustatic sea level rise and wave-induced shoreline erosion. As a result, transgressive barrier shoreline sands have a low potential for preservation in the rock record.
Figures & Tables
This lecture course is designed to provide geologic insights towards the development of depositional and exploration models for sandstone reservoirs associated with one or more of a variety of shelf and shoreline environmental settings. Sedimentologic and stratigraphic criteria will be utilized to more accurately predict the subsurface distribution and trend of reservoir quality sandstones. These criteria include a number of basic geologic “tools” such as well logs, cores, outcrop, seismic, and isopach and structure maps, all of which will be utilized in varying degrees during this course. Equally important in the development of models for shelf and shoreline sandstones is the subsurface analysis of modern depositional systems. An understanding of the three dimensional framework of modern clastic sedimentary environments is critical to the proper interpretation of vertical sequences, lateral facies relationships, sand body geometries and inhomogeneities of sandstone reservoirs.