| | Brian P. Coffey: Research |
 | | These Paleogene sediments are major aquifers, yet little is known concerning the facies distribution and diagenesis within the deeper portion of the basin. |
 | | A refined sequence stratigraphic model for the Paleogene mixed clastic-carbonate succession of the region will incorporate the wave-and ocean current-dominated setting, the widespread non-depositional, wave-abraded inner shelf (hardground), the near shore siliciclastic estuarine/lagoon/barrier systems, the echinoderm and bryozoan-rich outer shelf facies, and marine vs. fluvial incisional events into a non-tropical depositional framework. |
 | | The purpose of this study is to generate a high resolution sequence stratigraphic framework to document the stratigraphic signature showing climatic transition from greenhouse conditions of the early Eocene to the onset of icehouse conditions by the early Oligocene, as preserved in the strata of the southeast Atlantic Coastal Plain. |
| www.geol.vt.edu /gradstu/bcoffey/research.html (1452 words) |