Re-Evaluating the Origin of an Upper Eocene Diamictite in the Coastal Plain of East-Central Georgia: An Impactoclastic Layer?

Details Re-Evaluating the Origin of an Upper Eocene Diamictite in the Coastal Plain of East-Central Georgia: An Impactoclastic Layer? Re-Evaluating the Origin of an Upper Eocene Diamictite in the Coastal Plain of East-Central Georgia: An Impactoclastic Layer?

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1965h&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1965

Physics

Scientific paper

An unusual diamictite in the Upper Eocene stratigraphy of the Georgia
Coastal Plain previously has been interpreted as a volcaniclastic unit.
An initial re-evaluation of its origin suggests that the layer could be
related to a Late Eocene impact.

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