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The AAPG/Datapages Combined Publications Database

Houston Geological Society Bulletin

Abstract


Houston Geological Society Bulletin, Volume 48, No. 10, June 2006. Pages 19-19.

Abstract: Geochemical Logic and Techniques for Unconventional Previous HitGasNext Hit Exploration

By

Dan Jarvie
Humble Geochemical Services

Source rocks have been oil productive for many years, typically from highly fractured units or from adjacent porous intervals. In addition source rocks may be good resources for Previous HitgasNext Hit if they have the optimal organic richness and thermal maturity necessary to have converted both residual kerogen and any retained oil to Previous HitgasNext Hit. Obviously, completion engineering is a critical component of extracting the Previous HitgasNext Hit from these systems, but commercial rates will not be achieved if a minimum level of conversion or thermal maturity has not been reached.

While Previous HitgasNext Hit is generated in the oil window from all kerogen types (whether oil or Previous HitgasNext Hit prone), the presence of black oil components will occlude the limited permeability of a Previous HittightNext Hit shale system, resulting in low flow rates and precipitous decline rates. Thus, even though Previous HitgasNext Hit shows are present in the oil window and measured Previous HitgasNext Hit contents can appear commercial, it does not necessarily indicate the likelihood of commercial shale Previous HitgasNext Hit production. Previous HitGasNext Hit window thermal maturity is a critical component of producibility as the presence of higher molecular black oil components will occlude the limited permeability of a Previous HittightNext Hit source rock and result in low Previous HitgasNext Hit flow rates.

Thermal maturity should be assessed by both visual and chemical means. Visual methods such as vitrinite reflectance are the most common means and are widely used. Oftentimes, however, vitrinite reflectivity is not the best indication of the presence of producible Previous HitgasNext Hit from Previous HittightNext Hit rocks. These data should be complemented by data obtained through chemical techniques. These techniques include Rock-Eval Tmax, kerogen transformation ratio, Previous HitgasNext Hit composition, carbon isotopes, and residual liquids fingerprinting. Using these techniques, the extent of organic matter conversion to Previous HitgasNext Hit can be accurately determined. The key point is that indications of thermal maturity may not necessarily agree with the extent of kerogen conversion, nor provide a good indication of the presence of problematic compounds. Previous HitGasNext Hit risking plots can then be constructed to ascertain if all data provide a consistent assessment of Previous HitgasTop producibility.

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