Layered intrusions in East Greenland, mostly close to the contact between PreCambrian gneisses and Tertiary flood basalts, are commonly several million years younger than the flood basalts.
|Name||Title||Fields of interest|
|Elizabeth Ferriss||Postdoctoral Research Fellow|
|Ellen J. Crapster-Pregont||Graduate Research Assistant||moderate to high temperature and pressure geochemistry pertaining both to Earth's interior and meteorites.|
|Gary Mesko||Graduate Research Fellow|
|Geoffrey A. Abers||Associate Director - Seismology, Geology and Tectonophysics||Earthquake seismology, imaging and tectonics of active plate boundaries|
|Cornelia Class||Lamont Associate Research Professor||Solid Earth Geochemistry and Dynamics|
|Kerstin A. Lehnert||Senior Research Scientist||Geoinformatics, Scientific Data Management, Igneous Petrology, Geochemistry|