Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Diagenetic variations in Permo-Triassic Ivishak sandstone in Prudhoe Bay Field and central-northeastern National Petroleum Reserve in Alaska

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5992320
Porosity in the Ivishak sandstone on the North Slope is frequently cited as an example par excellence of secondary, or leached, porosity. In an attempt to corroborate and expand this contention, 100 thin sections were examined from representative wells in the Prudhoe Bay field and in NPRA. Monocrystalline quartz and biogenic chert are dominant framework grains in the two areas. Minor amounts of polycrystalline quartz, and sedimentary and metamorphic rock fragments are also present. Most of the chert in NPRA is nonporous, whereas Prudhoe Bay chert contains microscopic pores where siliceous biogenic debris, chalcedony, or dolomite formerly existed. The diagenetic sequence of the NPRA samples includes: (1) initial porosity loss by either compaction or siderite, chlorite, or pedogenic calcite cementation; (2) minor carbonate dissolution; (3) localized chert dissolution; and (4) quartz overgrowth formation. The diagenetic sequence of the Prudhoe Bay samples includes: (1) chert dissolution; (2) quartz overgrowth, kaolin, pyrite, and siderite formation; and (3) siderite dissolution.
Research Organization:
Exxon Co., Houston, TX
OSTI ID:
5992320
Report Number(s):
CONF-8505215-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 69:4
Country of Publication:
United States
Language:
English