| 791 - 805 |
Evaluation of the compositional changes during flooding of reactive fluids using scanning electron microscopy, nano-secondary ion mass spectrometry, x-ray diffraction, and whole-rock geochemistry
Zimmermann U, Madland MV, Nermoen A, Hildebrand-Habel T, Bertolino SAR, Hiotth A, Korsnes RI, Audinot JN, Grysan P |
| 807 - 829 |
Hydrocarbon-induced diagenetic alteration of the Permian White Rim Sandstone, Elate rite Basin, southeast Utah
Gorenc MA, Chan MA |
| 831 - 858 |
Factors controlling petroleum accumulation and leakage in overpressured reservoirs
Hao F, Zhu WL, Zou HY, Li PP |
| 859 - 888 |
The Paleozoic Hudson Bay Basin in northern Canada: New insights into hydrocarbon potential of a frontier intracratonic basin
Lavoie D, Pinet N, Dietrich J, Chen ZH |
| 889 - 925 |
Spontaneous potential: Key to understanding continuous and conventional gas in Upper Cretaceous sandstones, deep eastern Greater Green River Basin, southwest Wyoming
Bartberger CE, Pasternack I |
| 927 - 956 |
From shale oil to biogenic shale gas: Retracing organic-inorganic interactions in the Alum Shale (Furongian-Lower Ordovician) in southern Sweden
Schulz HM, Biermann S, van Berk W, Kruger M, Straaten N, Bechtel A, Wirth R, Luders V, Schovsbo NH, Crabtree S |
| 957 - 984 |
Multi-scale three-dimensional distribution of fracture- and igneous intrusion-controlled hydrothermal dolomite from digital outcrop model, Latemar platform, Dolomites, northern Italy
Jacquemyn C, Huysmans M, Hunt D, Casini G, Swennen R |
