| 989 - 1002 |
Reconstructing the architecture and sequence stratigraphy of the preserved fluvial record as a tool for reservoir development: A reality check
Miall AD |
| 1003 - 1029 |
Best practice stochastic facies modeling from a channel-fill turbidite sandstone analog (the Quarry outcrop, Eocene Ainsa basin, northeast Spain)
Falivene O, Arbues P, Gardiner A, Pickup G, Munoz JA, Cabrera L |
| 1031 - 1058 |
From petroleum-type organofacies to hydrocarbon phase prediction
di Primio R, Horsfield B |
| 1059 - 1088 |
Mass-transport complexes and associated processes in the offshore area of Trinidad and Venezuela
Moscardelli L, Wood L, Mann P |
| 1089 - 1119 |
Sea level influence on the nature and timing of a minibasin sedimentary fill (northwestern slope of the Gulf of Mexico)
Mallarino G, Beaubouef RT, Droxler AW, Abreu V, Labeyrie L |
| 1121 - 1140 |
High-resolution sequence-stratigraphic correlation between shallow-marine and terrestrial strata: Examples from the Sunnyside Member of the Cretaceous Blackhawk Formation Book Cliffs eastern Utah
Davies R, Howell J, Boyd R, Flint S, Diessel C |
| 1141 - 1143 |
Velocity-depth trends in Mesozoic and Cenozoic sediments from the Norwegian Shelf: Discussion
Japsen P |
| 1145 - 1148 |
Velocity-depth trends in Mesozoic and Cenozoic sediments from the Norwegian Shelf: Reply
Storvoll V, Bjorlykke K, Mondol NH |
