<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Thomas E. Moore</dc:contributor>
  <dc:creator>Christopher J. Potter</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>As part of the U.S. Geological Survey assessment of undiscovered oil and gas&#13;
resources in the National Petroleum Reserve-Alaska (NPRA), two structural plays were&#13;
assessed in thrust-faulted and folded Upper Cretaceous rocks of the Brookian&#13;
megasequence. These are the Brookian Topset Structural Play and the Torok Structural&#13;
Play, located in the Brooks Range foothills and the southern part of the coastal plain,&#13;
within the Tertiary-age frontal part of the Jurassic to Tertiary Brooks Range orogenic&#13;
belt. A new regional structural interpretation, developed through regional seismic&#13;
analyses, reconnaissance field investigations, and new thermal constraints, guided the&#13;
geologic evaluation and risking of these plays. Volumetric parameters were derived from&#13;
seismic reflection data, well data and oil and gas field analogs.&#13;
The fundamental elements of the Brookian Topset Structural Play, exemplified by&#13;
the undeveloped Umiat oil field, include: (1) reservoirs in Nanushuk Group and&#13;
uppermost Torok Formation shallow-marine to nonmarine sandstones draped over&#13;
anticlines caused by structural thickening in underlying Torok mudstones; (2) seals&#13;
provided by overlying shale drapes in the Nanushuk, and locally by thrust faults; (3)&#13;
Torok, gamma-ray-zone (GRZ) or pebble shale source rocks; (4) remigration of&#13;
hydrocarbons from early formed (Late Cretaceous) stratigraphic traps disrupted by 60 Ma&#13;
thrusting, into newly formed structural traps. The 60 Ma thrusting was probably&#13;
accompanied by new generation and migration of natural gas resulting from late&#13;
structural thickening and tectonic loading. Subsurface data from the Umiat field and&#13;
other seismic reflection data within the play area indicate that the structural traps are&#13;
commonly compartmentalized by thrust faults.&#13;
The fundamental elements of the Torok Structural Play, exemplified by the&#13;
undeveloped East Kurupa gas accumulation just south of NPRA, include: (1) reservoirs&#13;
in lower Torok Formation basin-floor sandstones, and perhaps in small sandstone bodies&#13;
intercalated with middle to upper Torok mudstones; (2) structural traps provided by&#13;
folded sandstone bodies above thrust faults within a pervasively deformed passive-roof&#13;
duplex beneath the foothills and a less-strongly deformed domain to the north; (3) seals&#13;
provided by Torok mudstone, both stratigraphically above the sandstone bodies and&#13;
smeared along bounding thrust faults; (4) Torok, GRZ, pebble shale, or Kingak Shale&#13;
source rocks; (5) a migration and charging scenario similar to that of the Brookian Topset&#13;
Structural Play. According to our estimates, the Brookian Topset Structural Play contains 137&#13;
million barrels of technically recoverable oil and 10.6 trillion cubic feet (TCF) of&#13;
technically recoverable, non-associated natural gas, with both values representing the&#13;
mean estimate (expected value). The Torok Structural Play contains about 35 million&#13;
barrels of technically recoverable oil and 17.9 TCF of technically recoverable, nonassociated&#13;
natural gas.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr03266</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Brookian structural plays in the National Petroleum Reserve, Alaska</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>