USGS · 70044329
Structural evolution of the southeastern portion of the Anadarko Basin region
Abstract
Field investigations in the Lake Classen-Turner Falls, Oklahoma, area of the northern Arbuckle anticline, on the southeastern margin of the Anadarko basin, indicate that transpressional (oblique compressional) deformation of Late Pennsylvanian age dominated the structural development of this area. The Arbuckle anticline is detached along the NW -trending, SW -dipping, left-reverse Arbuckle fault and is thrust obliquely onto the margin of the Tishomingo block to the east. Paleostress analysis of slip lines on mesoscopic faults along the northeastern limb of the Arbuckle anticline, associated in style and geometry with oblique Arbuckle thrusting, indicates compression directed N. 35-60° E.
Explore related subjects
Keep this discovery
Explore connections, maps & timelines
William J. Perry. 1989. Structural evolution of the southeastern portion of the Anadarko Basin region. https://pubs.usgs.gov/publication/70044329
Cite the original work for its findings. Save a collection to share your selection of sources.