Abstract. The present study of field, petrological, exploration well, and seismic data describes backward-dipping duplexes comprised phyllitic coal bedding-parallel décollements thrusts localized along lithological transitions in tectonically thickened Lower Devonian to lowermost Upper Devonian; uppermost Devonian–Mississippian; Pennsylvanian–lowermost Permian sedimentary strata the Wood Bay an...
