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Houston Geological Society Bulletin

Abstract


Houston Geological Society Bulletin, Volume 49, No. 2, October 2006. Pages 11-11.

Abstract: Norphlet Aeolian Dunes in the Deep Water Gulf of Mexico

By

Ted Godo
Senior Staff Geologist
Shell Exploration & Production Co.

The prolific Norphlet aeolian sand play, sealed and sourced by the basal Smackover, has been exploited for its oil and gas reserves both onshore and in the offshore Gulf of Mexico waters. The onshore trend extends from near Jackson, Mississippi, at the Pisgah anticline, southeastward over Hatter’s Pond field in Alabama and into the Florida panhandle at Flomaton/Jay field. The offshore gulf trend begins in the waters of Mobile Bay and extends offshore southeast into the Destin Dome area offshore Florida and southward into the Desoto Canyon protraction area. Norphlet exploration in the Destin Dome protraction area was active from the mid 1980s through the early 1990s. Despite some success the prospects were never commercialized owing to poor economics and environmental reasons. The last federal lease sale that included this area was held in 1988.

In December 2001, Federal Lease Sale 181 opened a small area of the eastern gulf encompassing 100 Outer Continental Shelf (OCS) blocks in the Desoto Canyon and Lloyd Ridge protraction areas. In anticipation of this sale, Shell initiated a regional geologic and Previous HitgeophysicalTop interpretation, which indicated that Norphlet aeolian sands would very likely occur in the northern portion of the Sale 181 area. Prospect Shiloh was mapped in Desoto Canyon in 7500 feet of water and geologically positioned downdip of the Cretaceous shelf/Florida escarpment edge. Shiloh’s exploration targets were stacked Jurassic age objectives of the Cotton Valley, Haynesville and Norphlet Formations in a four-way dip closure.

This presentation focuses on the characteristics of the Norphlet oil discovery at Shiloh and its impact on the regional understanding of this play. Just as in the onshore trend, the Smackover provided the source rock and seal. A Norphlet whole core was found to be composed entirely of an aeolian dune complex with chlorite-coated grains that had better porosity than fields in Mobile Bay. Detailed petrography revealed interesting similarities and differences with other segments of this play. Verification of the Norphlet presence, quality and charge in the deep water has opened up a new play in the Gulf of Mexico. Further exploration in Desoto Canyon is scheduled for 2007.

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