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The AAPG/Datapages Combined Publications Database

GCAGS Transactions


Gulf Coast Association of Geological Societies Transactions
Vol. 53 (2003), Pages 363-373

The Regional Geothermal Heat Flow Regime of the North-Central Gulf of Mexico Continental Slope

Michael L. Jones, Seiichi Nagihara, Michael A. Smith


Eighty-eight oil and gas wells in the Texas-Louisiana continental slope were analyzed to obtain heat flow and geothermal gradient values. Heat flow values at 55 of these wells were determined in order to provide a basis for modeling hydrocarbon maturity. The geothermal gradient was calculated for all wells. Heat flow was obtained as the product of the geothermal gradient and thermal conductivity of the sediments. The thermal gradient was obtained from bottom-hole temperatures (BHTs). The Hornor plot method was used to correct BHTs when there were multiple measurements obtained at the same depth but different times. For single measurements, a Previous HitcorrectionNext Hit scheme that utilizes the relationship between temperature, depth and shut-in time was used. The conductivity was estimated from petrophysical logs by a two-step procedure: first, determining lithology using a volume of shale calculation and then calculating the bulk conductivity using the Previous HitgeometricTop mean law. Radiogenic heat production within the sediments was constrained at some of the wells using natural gamma spectrometer (NGS) logs. A method, which utilizes the relationship between the total gamma ray log and heat production, was used for the other wells.

The heat flow values from this study and heat flow probe data obtained previously show regional trends that appear to be influenced by two factors: accumulation rate of recent sediments and proximity to diapiric salt structures. High sedimentation rates in the Mississippi submarine fan have suppressed surface heat flow. Salt domes in the upper continental slope elevate heat flow, but the presence of laterally continuous salt sheets appears to have little effect on heat flow.

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