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Use of Iodine Surface Geochemistry for Exploration of Cretaceous Age D and Muddy Channels in the Denver and Powder River Previous HitBasinsNext Hit

Tedesco, Steven A.
Atoka Geochemical Services Corp, Englewood, CO

The concept of surface geochemistry as an exploration tool to find new Previous HitpetroleumNext Hit reservoirs is based on the concept of vertical migration. Based on this concept, Previous HitpetroleumNext Hit migrates to the surface from a Previous HitpetroleumNext Hit reservoir at depth along micro-pores, micro-fractures and micro-unconformities. The Previous HitpetroleumNext Hit compounds and their by-products in the soil substrate will eventually vent to the atmosphere where they are broken down by plant and bacterial action and react with other elements and compounds. The presence or absence of anomalous surface geochemical conditions directs the explorationist to either proceed forward to define a prospect with potential drilling or to abandon the prospect. Surface geochemistry, if done properly, inherently reduces risk and increases success.

Iodine has a unique association with thermally cracked hydrocarbons. Where Previous HitpetroleumNext Hit is present in the soil or in the subsurface anomalous amounts of iodine are present. Analyzing for iodine allows for a cost effective exploration tool to locate and define the approximate location of Silurian Age reefs in the subsurface. This allows a more effective use of exploration dollars in shooting seismic and leasing. Examples of successful iodine surveys will be presented from the Denver and Powder River Previous HitBasinsNext Hit where iodine has been effectively to find new Previous HitpetroleumTop reserves.