Structural controls on Late Cambrian and Early Ordovician carbonate sedimentation in eastern Kentucky.

Abstract

Establishes the subsurface distribution and lithofacies variation of the Cambro-Ordovician Knox Supergroup and the Ordovician Ottawa Supergroup (excluding Trenton Group). The rejuvenation of depocenters which actively influenced lithofacies variation and distribution can explain the lithostratigraphic trends and relationships. -from Authors