FUTURE TASKS FOR 10/05 - 3/O6 Complete integration of stratigraphy task with structure task and finalize isopach maps in November. Integrate stratigraphy.

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FUTURE TASKS FOR 10/05 - 3/O6 Complete integration of stratigraphy task with structure task and finalize isopach maps in November. Integrate stratigraphy with petrography and refine depositional model. Integrate with other tasks to develop areas of potential exploration interest. Conduct detailed field studies (York field and Harlem field) Write final report in 2/06 to 3/06.

OUTLINE Stratigraphic framework of Middle and Late Ordovician. Paleogeography and facies mapping. Log signature of mapped facies across the basin. Cross sections illustrating facies distribution across the basin. Regional isopach maps of Cambrian-Ordovician Basin architecture Relationship of isopach maps to producing trends Summary and Conclusions

Williams County, OH Permit Clean carbonate with sharp upper contact UTICA TRENTON BLACK RIVER

Marion County, OH Permit 196 Sub basin facies UTICA PT.PLEASANT LEXINGTON LOGANA CURDSVILLE BLACK RIVER KNOX

Warren County, OH Permit Sub-basin facies UTICA LEXINGTON LOGANA CURDSVILLE BLACK RIVER KNOX PT. PLEASANT

Steuben County, NY Permit Argillaceous carbonates with sharp upper contact TRENTON BLACK RIVER KNOX UTICA

Pike County, KY Permit Argillaceous carbonate with gradational upper contact Pt. Pleasant Lexington Logana Curdsville Black River

Trenton Black River Pendleton County, WV Permit 6 Clean carbonates that have been overthrust

NWSW D_D ORDV SH KOPE UTCA TRNN BKRV GLRV KNOX VE=200X

NWSED_H ORDV SH KOPE UTCA TRNN BKRV GLRV KNOX

NW SE D_J ORDV SH KOPE UTCA TRNN BKRV KNOX

NWSED_L ORDV LRNE UTCA PNPL TRNN BKRV KNOX TRNN BKRV PCMB

SWNE ORDV LRNE UTCA TRNN BKRV KNOX

SUMMARY AND CONCLUSIONS Exploration potential exists along the platform margin. Grainstones in skeletal shoals along platform margin that wraps around from IN-OH- ONT-PA appear to have some of the best reservoir quality (Lake Erie region has great potential). Best facies for hydrothermal reservoirs appear to be in clean Trenton and Black River carbonates. Area of western NY that contains a clean upper Trenton carbonate may have potential for hydrothermal reservoir facies. Localized areas of clean carbonate buildups deeper in the basin and off the platform region are present and are potential targets. Areas that contain a clean Trenton with a sharp upper contact may be imaged seismically to identify potential exploration trends?