859 - 872 |
Geological risk mapping and prospect evaluation using multivariate and Bayesian statistical methods, western Sverdrup Basin of Canada Chen ZH, Osadetz KG |
873 - 885 |
Diagenetic modeling to assess the relative timing of quartz cementation and brittle grain process during compaction Makowitz A, Lander RH, Milliken KL |
887 - 907 |
Contrasting thermal evolution of thrust systems: An analytical and modeling approach in the front of the western Alps Deville E, Sassi W |
909 - 920 |
Oil quality in deep-water settings: Concerns, perceptions, observations, and reality Katz BJ, Robison VD |
921 - 938 |
The controls on the composition of biodegraded oils in the deep subsurface: Part II - Geological controls on subsurface biodegradation fluxes and constraints on reservoir-fluid property prediction Larter S, Huan H, Adams J, Bennett B, Jokanola O, Oldenburg T, Jones M, Head I, Riediger C, Fowler M |
939 - 962 |
Thermal conductivity and radiogenic heat production of sedimentary and magmatic rocks in the Northeast German Basin Norden B, Forster A |
963 - 966 |
Mississippian Barnett Shale, Fort Worth basin, north-central Texas: Gas-shale play with multi-trillion cubic foot potential: Discussion Ewing TE |
967 - 969 |
Mississippian Barnett Shale, Fort Worth basin, north-central Texas: Gas-shale play with multi-trillion cubic foot potential: Reply Montgomery SL, Jarvie DM, Bowker KA, Pollastro RM |
971 - 973 |
Climatic significance of Holocene beachrock sites along shorelines of the Red Sea: Discussion Mozley PS, Burns SJ |
975 - 982 |
Climatic significance of Holocene beachrock sites along shorelines of the Red Sea: Reply Friedman GM |