General Field Information |
Produces Oil: Yes Produces Gas: Yes |
Geologic Province: |
Western Flank of the Central Kansas Uplift |
Exploration Method: |
Subsurface and Geophysical |
Surface Formation: |
Cretaceous |
Oldest Formation Penetrated: |
Arbuckle |
Drilling Casing Practices: |
Standard rotary drilling practices were utilized with a chemical mud system. Minimum penetration of the Mississippian reservoir is desirable for open hole completion. Generally only three feet is necessary. Mud properties when nearing the "Pay" section average 38 viscosity, 9.4 weight, and 10 cc. water loss.
5 1/2" Production Casing is set for open hole completion with a D. V. tool at approximately 1600', adjacent to the Stone Corral Anhydrite. Acidize if necessary, by "dumping" 250 gallons 15% and loading the casing. |
Electric Logging Practices: |
Gamma Ray-Neutron-Resistivity with Caliper, 5" or detailed from total depth to 100' above the Heebner Shale, 2" out of hole to "grass roots." |
Discussion: |
The Don Field is located within the northwest-southeast trending Spergen subcrop of the Mississippian Meramecian Series. Approximately 125' post Osage rocks are present in this area. (65' Warsaw and 60' Spergen). Excellent oil and gas reserves have been found along and within the Spergen sub-crop from Comanche County, in southern Kansas, to as far north as Gove County, in west-central Kansas.
The more significant Fields controlled by stratigraphic and structural traps from southest to northwest include:
Shimer and Wilmore in Comanche County
Alford in Comanche and Kiowa counties
Fralick West and Martin in Kiowa County
Pleasant Valley in Ford County
Mellecker, Far, Purdyville, Bindley, Hallet and Starrett in Hodgeman, Guzzlers Gulch, Laird, Aldrich, Aldrich Northeast, Dickman, Arnold, Southwest and Judica in Ness County
Lungren Field in Gove County. |
|
Depth Top: |
4702 feet |
Geological Age: |
Mississippian |
Depositional Environment: |
After deposition of the Mississippian Spergen rocks the area was subjected to uplift and erosion. Subsequent deposition of the younger overlying Pennsylvanian beds altered the strata with further deformation. THe productive Mississippian Spergen area's or "highs" are composite structural and topographic features. |
Formation Lithology: |
Mississippian Spergen Dolomite: non cherty, cream to tan, finely to medium crystalline, sucrosic; with inter-crystalline, vugular, and some fossil-cast porosity; and containing the Foraminifer Endothyra Baileyi. Infrequently grading laterally into cream, medium crystalline, dense, non-cherty limestone. |
Formation Geometry: |
Mississippian (Spergen): Truncated Mississippian rocks dip gently westward into the Hugoton Embayment of the Anadarko Basin. "Mounds" of eroded Spergen dolomite are found within the boundaries of the northwest southeast trending anticlinal structure. |
Trap Type: |
Structural closure on a northwest-southeast trending anticline. |