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Ahead of Print Abstract
AAPG Bulletin, Preliminary version published online
Copyright © 2025. The American Association of Petroleum Geologists. All rights reserved.
DOI:10.1306/10212524062
Analysis of anomalous thicknesses of the Hunton Group (Late Ordovician - Early Devonian) using image and standard open-hole 
wireline
logs
wireline logsChase Watkins and James Puckette
Ahead of Print Abstract
wireline logs that accompany these anomalies. By integrating data from resistivity image logs, wireline log curves, and isochore maps, anomalous thickness patterns can be explained by depositional variation and erosion, without relying on interpretations of faults intersecting the wellbores. Patterns in isochore maps strongly suggest that vertical movement on 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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