24 Energy Resources of the Paleozoic I
Friday, 28 March 2003
8:40 AM - 12:00 PM
THE TRENTON-BLACK RIVER PLAY -- AN HISTORICAL PERSPECTIVE
Paper number: 24-1
Program: THEME SESSIONS
Time: 8:40 AM – 9:20 AM
Authors
Abstract
Two small linear Ordovician fields in southeastern Michigan, Deerfield and Northville, were discovered in 1936 and 1954, respectively, but the next significant Ordovician discovery was the Albion-Scipio trend in southern Michigan. The Ordovician reservoir at north end of the Albion-Scipio trend was actually drilled in 1943, but the well was plugged back to the Devonian. The impetus for drilling the discovery well, completed in early 1957, was due to a vision by a practicing psychic, not geology.
The combination of long periods without success interspersed with a few spectacular discoveries have continued to feed explorationists’ dreams of finding more Trenton-Black River reservoirs. The last 20 years of successes in southwestern Ontario and the most recent events in New York and West Virginia have shown that, for once, geology has an important role in this exploration. An understanding of regional tectonics to predict probable basement-related fault and fracture zones coupled with modern geophysical methods has proven an effective exploration strategy; however, finding these reservoirs still remains elusive and unpredictable.