Analysis Reactions Morphology by P.-J. Madec, E. Marechal, J.-E. Mark, T. Otsu, R.W.

By P.-J. Madec, E. Marechal, J.-E. Mark, T. Otsu, R.W. Richards, J.P. Queslel, T. Sato, B. Tieke

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Assoc. , v. 82, no. 2, p. 291-316. , 1974, Time-temperature relation in oil genesis: Am. Assoc. • v. 58, no. 12, p. 2516-2521. , Sass, J. , Lachenbruch, and R. F. DeRito, 1992, Heat flow and subsurface temperature as evidence for basin scale groundwater flow, North Slope of Alaska: Geol. Soc. America Bull, v. 104, no. 5, p. 528-542. , v. 105, no. 3, p. 675-691. , 1967, Thermal regime of a large diameter borehole: instability of the water column and comparison of air- and water-filled conditions: Geophysics, v.

_. _. __ Sprague Lewis #1 ___________________ 1~~UQL~~2~~~J 152-1219m [500-4000'] 1402-1448m [4600-4750'] 1463-1478m [4800-4850'] 1485-1494m [4871-4900'] 1494-1509m [4900-4950'] 1219-1719m (4000-5641') ____ J2J________ _________ ___ _ Conductivity values in (bIllCkels] are inferred values for a heat flow of 28 mW/m'. 10 W/rnK.. 40 W/rnK.. Thus the shale conductivity values are almost identical for samples with widely different densities. These figures also are consistent with the only moderately higher thermal gradients observed in the shale sections.

1, p. 21-32. Brigaud, F. , Chapman, D. , 1990, Thermal conductivity in sedimentary basins predicted from lithologic data and geophysical logs: Am. Assoc. , v. 74, no. 9, p. 1459-1477. , and Conaway, J. , 1984, Temperature gradient measurements in boreholes using low noise high resolution techniques: Geol. Survey Canada Current Research, Pt. B, Paper 84-lB, p. 101-108. , 1998, Heat flow and thermal history of the Anadarko Basin, Oklahoma: Am. Assoc. , v. 82, no. 2, p. 291-316. , 1974, Time-temperature relation in oil genesis: Am.

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