The National Petroleum Reserve in Alaska (NPRA) has been the focus of oil exploration during the past decade, stimulated by the mid-1990s discovery of the adjacent Alpine field—the largest onshore oil discovery in the United States during the past 25 years. Recent activities in NPRA, including extensive 3–D seismic surveys, six Federal lease sales totaling more than $250 million in bonus bids, and completion of more than 30 exploration wells on Federal and Native lands, indicate in key formations more gas than oil and poorer reservoir quality than anticipated. In the absence of a gas pipeline from northern Alaska, exploration has waned and several petroleum companies have relinquished assets in the NPRA.
This fact sheet updates U.S. Geological Survey (USGS) estimates of undiscovered oil and gas in NPRA, based on publicly released information from exploration wells completed during the past decade and on the results of research that documents significant Cenozoic uplift and erosion in NPRA. The results included in this fact sheet—released in October 2010—supersede those of a previous assessment completed by the USGS in 2002.
Recent Exploration Drilling
Most wells drilled during recent NPRA exploration, whose initial drilling season occurred in 2000, are within 50 miles of the Alpine oil field and targeted the Alpine sandstone, the main reservoir in Alpine field (Figure 1). The stratigraphic interval including the Alpine sandstone was assessed as the Beaufortian Upper Jurassic play in the USGS 2002 assessment of NPRA.
Alpine Sandstone - Northeastern NPRA
Five discoveries of oil have been reported in the Alpine sandstone in northeastern NPRA (Figure 2). Alpine West, Lookout, and Pioneer are oil accumulations with little or no free gas. A fourth discovery, Mitre, appears to be predominantly a gas accumulation with an oil leg in the south (Figure 2). The fifth discovery, the Spark-Rendezvous accumulation, is a much larger reservoir system that includes gas plus condensate at shallower depths in the north and oil at greater depths in the south (Figure 2).
Significantly, the Spark-Rendezvous accumulation represents an abrupt transition of hydrocarbon phase within the Alpine sandstone—from oil on the east to gas on the west. Most known or inferred hydrocarbon accumulations west of Spark-Rendezvous are gas. This transition occurs just 15 to 20 miles west of the Alpine oil field and is not related to the structural position of the reservoir (Figure 2). Tests of gas flow rates and volumes are not known to have been conducted west of the Spark-Rendezvous accumulation.
Although the data released are insufficient to make a precise calculation of the volume of oil and gas discovered, we estimate that 120 to 200 MMBO (including oil and condensate) and 1.9 to 3.0 TCFG may be technically recoverable from these accumulations. The Spark-Rendezvous accumulation is so large that if it were entirely oil, it would rival or exceed the Alpine field in recoverable resources.
Several recently drilled wells, most located west and northwest from the Spark-Rendezvous accumulation, evaluated other stratigraphic intervals, including (from oldest to youngest) the Triassic Ivishak Sandstone (Ellesmerian Ivishak play in the USGS 2002 assessment of NPRA), lower Kingak Shale (Beaufortian Lower Jurassic Topset play), uppermost Kingak Shale (Beaufortian Cretaceous Topset play), and the Torok Formation (Brookian Clinoform play). One well in the Ellesmerian Ivishak play and two wells in the Beaufortian Cretaceous Topset play are dry holes. At least four wells in the Beaufortian Lower Jurassic Topset play encountered gas shows but no indications of recoverable oil. Two wells in the Brookian Clinoform play encountered oil-saturated sandstone with poor reservoir quality and were not tested (Figure 2; Kokoda). Also, two wells (Spark 4 and Hunter; Figure 2) that targeted the Alpine sandstone encountered thin intervals of oil-saturated sandstone in the Brookian Topset play. Seven wells drilled west of Spark-Rendezvous remain proprietary (figs. 1 and 2); we infer that these are either gas shows or dry holes based on the predominance of gas in wells lower on structure, relinquished leases, and company divestiture of assets.
Gubik and East Umiat: Southeastern NPRA
In southeastern NPRA, one recently drilled well at the Wolf Creek gas accumulation (discovered in 1951) remains proprietary. Just outside the southeastern boundary of NPRA, two wells were drilled recently at the Gubik gas accumulation (discovered in 1963) and another well, located near the East Umiat gas accumulation (discovered in 1964), was drilled to a deeper target. One of the recent Gubik wells indicates producible gas. The other recent Gubik well and the deeper test at East Umiat remain proprietary. These wells drilled in the Brooks Range foothills add no information to indicate the need for updating the 2002 USGS assessment of plays in southern NPRA.
Cenozoic Uplift in NPRA
Cenozoic uplift and erosion (from about 60 to 15 million years ago) of the Brooks Range foothills in southern NPRA and of a broad area in northern NPRA (Figure 1) may provide an explanation for the unanticipated predominance of gas in the Alpine sandstone and other strata. The magnitude and timing of uplift and erosion have been estimated by using sonic logs from exploration wells (Figure 1) and additional geological evidence. The uplift and erosion caused a decrease in confining pressure on subsurface fluids, resulting in expansion of free gas in reservoirs, degassing of oil in reservoirs, and degassing of formation water.
Geologic History of Oil and Gas Generation
Oil generation and most gas generation were complete across NPRA by about 90 million years ago. Thus, at the time of Cenozoic uplift and erosion, it is likely that oil was present in various reservoirs in northern NPRA (lower thermal maturity) and that gas was present in various reservoirs in southern NPRA (higher thermal maturity). In areas of modest uplift in northeastern NPRA, degassing of oil accumulations likely generated gas caps and displaced oil downward into poorer quality reservoir rocks (for example, Spark-Rendezvous). In areas of moderate uplift in northwestern NPRA and significant uplift in southern NPRA, degassing of oil combined with significant gas expansion likely caused a gas “flush” outward, away from the uplifted areas. Oil degassing and gas expansion likely explain the abrupt oil-to-gas transition in the Alpine sandstone in northeastern NPRA. Significantly, evidence of oil saturation in Brookian stratigraphic plays west of the oil-to-gas transition (Figure 2) suggests that Brookian rocks may have been shielded from these processes and may retain potential for undiscovered oil across northern NPRA.