Thermal History of the Chesapeake Bay Impact Crater
Anomalously high groundwater salinities exist within the syn-impact sediment of the Chesapeake Bay impact crater, including an unexplained brine. This brine may be the result of phase-separation of seawater that occurred within the syn-impact sediments as underlying deformed and possibly melted base...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Others |
| Published: |
Virginia Tech
2011
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10919/9980 http://scholar.lib.vt.edu/theses/available/etd-06092004-173945 |