Conclusions
- On a gross scale, major rock types show predictable distribution patterns throughout the Panoma Field.
- Thinning in the marine rocks to the northwest is compensated by thickening in the nonmarine intervals. Overall thickness of the Council Grove is relatively consistent throughout Panoma.
- The influx of quartz silt, very fine sand and clay from the west and northwest is quite dramatic, on a regional scale, and is evident in both the nonmarine and marine intervals.
- Better marine carbonates reservoir rocks tend to be concentrated in the in the central and southeast portions of Panoma.
- Conversely, better nonmarine reservoir rocks tend to be concentrated in the west and northwestern portion of the Panoma field