Little Rock, Arkansas, United States
6-8 April 2017
The objective of this field trip is to examine the deposits of an upper slope and slope canyon to deep basin floor deepwater depositional system developing along a Pennsylvanian-age fold and thrust belt called the Ouachita Trough. The units under study are part of the Stanley Group, Jackfork Group and the overlying Atoka Group.
Added on 05 December, 2016