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DOI:10.1306/10212524062
Analysis of anomalous thicknesses of the Hunton Group (Late Ordovician - Early Devonian) using image and standard open-hole wireline logs
Chase Watkins and James Puckette
Ahead of Print Abstract
fault
blocks created differential accommodation, with increased deposition along downthrown fault blocks and nondeposition and erosion on uplifted fault blocks. The most significant consequence of this study is the realization that any attempt to understand the fault
movement and paleotopography during the Hunton Group must also include the underlying Sylvan Shale as Hunton deposition was influenced by the post-Sylvan paleotopography.
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