| Structure: | STEEP REGIONAL S DIP TO CARBONIFEROUS FORMATIONS. OVERTHRUST BLOCK CUT BY NE TEAR FAULTS, BEDDING PLANE FAULTS, AND N-S FAULTS WITH WEST SIDE MOVING RELATIVELY NORTH. TWO TYPES OF SMALL FOLDS FORMED BY E-W COMPRESSION. ; REG.TRENDS: THRUST FAULTING FROM S IN LATE PALEOZOIC. |