| 205 - 215 |
A new oil-window indicator? The magnetic assemblage of claystones from the Baffin Bay volcanic margin (Greenland)
Abdelmalak MM, Aubourg C, Geoffroy L, Laggoun-Defarge F |
| 217 - 233 |
Carbonate porosity creation by mesogenetic dissolution: Reality or illusion?
Ehrenberg SN, Walderhaug O, Bjorlykke K |
| 235 - 244 |
Probabilistic correlation of single stratigraphic samples: A generalized approach for biostratigraphic data
Punyasena SW, Jaramillo C, de la Parra F, Du YL |
| 245 - 275 |
Petrological and geochemical investigations of potential source rocks of the central Congo Basin, Democratic Republic of Congo
Sachse VF, Delvaux D, Littke R |
| 277 - 300 |
Quantification of static connectivity between deep-water channels and stratigraphically adjacent architectural elements using outcrop analogs
Funk JE, Slatt RM, Pyles DR |
| 301 - 314 |
Tectonic geomorphological investigations of antiforms using differential geometry: Permam anticline, northern Iraq
Burtscher A, Frehner M, Grasemann B |
| 315 - 336 |
Hydrodynamic aquifer or reservoir compartmentalization?
Muggeridge A, Mahmode H |
| 337 - 354 |
Source of molten elemental sulfur and hydrogen sulfide from the Inigok well, northern Alaska
Kaplan IR, Bird KJ, Tailleur IL |
| 355 - 374 |
Innovative methods for flow-unit and pore-structure analyses in a tight siltstone and shale gas reservoir
Clarkson CR, Jensen JL, Pedersen PK, Freeman M |
| 375 - 390 |
Origins of gypsum in deep carbonate reservoirs: Implications for hydrocarbon exploration and production
Amadi FO, Major RP, Baria LR |
