SEDIMENT PROVENANCE FOR CARBONIFEROUS OUACHITA-ARKOMA AND BLACK WARRIOR BASINS USING DETRITAL MUSCOVITE 40AR/39AR GEOCHRONOLOGY AND SANDSTONE COMPOSITIONAL ANALYSIS
40Ar/39Ar Detrital ages from the Ouachita-Arkoma Basins (n>1500) show distinct characteristics that are represented throughout samples from both the Late Mississippian and the Early Pennsylvanian. A dominant Taconic mode is constant throughout all samples from the Ouachita-Arkoma region. Two subordinate Acadian modes are often defined at ca. 370 Ma and 400 Ma. In the initial samples from the Black Warrior Basin, a younging upward progression is evident from the gradual shift from a prominent Taconic mode to Acadian and eventual Alleghanian mode higher in the section.
Significant similarities are observed between the two regions, such as the two subordinate Acadian modes at ca. 370 Ma and 400 Ma and the dominant Laurentian crustal signature. Noticeable differences in the detrital signatures is expressed by the lack of an Alleghanian mode in the Ouachita-Arkoma Basin samples and the presence of a constant Taconic peak in the Ouachitas that disappears in the higher section of the Black Warrior Basin. A few Pan-African aged grains from the Ouachita region suggests a possible secondary Gondwanan source. The dominant Laurentian crustal signature, indicated in both forelands, implies a primary Laurentian source of detritus transported by multiple complex axial drainage systems.