GEOCHEMICAL COMPARISON OF OILS FROM UPPER PENNSYLVANIAN KANSAS RESERVOIRS, NW KANSAS TO WOODFORD SHALE SOURCE ROCKS: A CASE FOR LONG DISTANCE MIGRATION
Previous studies of Woodford oils and source rocks in the Anadarko Basin yield a clearly defined set of biomarker characteristics. In particular Woodford oils and source rock extracts have a unique distribution of arylisoprenoids derived from green sulfur bacteria that thrived under the euxinic conditions of deposition prevalent during the formation of the Woodford. Along with the other families of biomarkers, these arylisoprenoids provide a powerful oil/source rock correlation tool. The geochemical characteristics of the oils found in the Upper Pennsylvanian Lansing-Kansas City (LKC) formation are consistent throughout western Kansas and similar to those found in the oils from the Anadarko Basin in Oklahoma. It has been proposed previously that the LKC oils originated from the Late Devonian Woodford (Chattanooga) Shale in the deep Anadarko Basin and underwent long distance migration to the reservoirs in NW Kansas. The LKC oils show strong similarities to both Woodford sourced oils and rock extracts in the Anadarko Basin supporting the concept of long distance migration. As a part of this study, an investigation into the organic rich shales within the LKC in NW Kansas is being undertaken as these shales may contribute to the overall oil composition.