631 - 661 |
Sedimentology, stratigraphy, and reservoir properties of an unconventional, shallow, frozen petroleum reservoir in the Cretaceous Nanushuk Formation at Umiat field, North Slope, Alaska Shimer GT, McCarthy PJ, Hanks CL |
663 - 694 |
Effect of pore structure on the producibility of tight-gas sandstones Sakhaee-Pour A, Bryant SL |
695 - 728 |
Geologic and seismic modeling of a coarse-grained deep-water channel reservoir analog (Black's Beach, La Jolla, California) Stright L, Stewart J, Campion K, Graham S |
729 - 763 |
A comparative study of reservoir modeling techniques and their impact on predicted performance of fluvial-dominated deltaic reservoirs Deveugle PEK, Jackson MD, Hampson GJ, Stewart J, Clough MD, Ehighebolo T, Farrell ME, Calvert CS, Miller JK |
765 - 791 |
Dolomites of the Boat Harbour Formation in the Northern Peninsula, western Newfoundland, Canada: Implications for dolomitization history and porosity control Olanipekun BJ, Amy K, Brand U |
793 - 824 |
Assessing the internal character, reservoir potential, and seal competence of mass-transport deposits using seismic texture: A geophysical and petrophysical approach Alves TM, Kurtev K, Moore GF, Strasser M |
825 - 849 |
Structural analysis of a salt-cored transfer zone in the South Timbalier Block 54, offshore Gulf of Mexico: Implications for restoration of salt-related extensional structures Bose S, Mitre S |
851 - 857 |
Modern internal waves and internal tides along oceanic pycnoclines: Challenges and implications for ancient deep-marine baroclinic sands: Discussion Dunham JB, Saller A |
858 - 879 |
Modern internal waves and internal tides along oceanic pycnoclines: Challenges and implications for ancient deep-marine baroclinic sands: Reply Shanmugam G |