Cooperative Agreement on Energy Technologies: Fluids Migration in the Brooks Range
DE-FC26-01NT41248 (Task 3.04.2)
The overall goals of this project are to:
- Develop a model of when and where fractures developed in the Colville basin in order to better predict oil and gas migration pathways, timing of hydrocarbon migration, and timing of trap formation.
- Improve exploration models by providing a clearer understanding of the timing and distribution of hydrocarbon generation and migration, that will ultimately lead to the discovery of additional hydrocarbon reserves in northern Alaska.
University of Alaska, Fairbanks, AK
Project insights include:
- Two transects through the Brooks Range foothills into the adjacent Colville basin are nearing completion. These two transects illustrate the two main structural styles of the Brooks Range rangefront—a complex frontal duplex/triangle zone in the west and a simpler passive roof duplex in the east.
- Four main fracture sets have been identified in both transects: an early filled fracture set related to regional stresses prior to folding and thrusting; a later filled fracture set that formed during thrusting; and two younger, unfilled fracture sets that are related to late folding and/or uplift and unroofing.
- Apatite fission track ages suggest that deformation and uplift have been episodic during the late Cretaceous and early Tertiary, with different parts of each transect active at any one time.
- Thermal data from fracture fill implies that the early filled fractures filled at temperatures exceeding that of oil generation, implying that these fractures would not be good exploration targets.
- In general, the present-day maximum horizontal in situ stress within the Colville basin is oriented north-northwest, perpendicular to the deformation front. However, stress trajectories become more complex adjacent to and overlying the Barrow Arch, suggesting interference with basement structure and/or the nearby rift margin.
The goal of this project is to develop a new and clearer picture of when and where fractures developed during the evolution of the Colville basin and adjacent Brooks Range foothills in order to better predict the timing and location of fracture-enhanced reservoirs, and the timing, orientation, and depth of oil and gas migration pathways. This in turn will improve understanding of the North Slope petroleum systems.
Much of Alaska’s governmental and private economies revolve around the petroleum industry. However, recent years have seen production declines from Prudhoe Bay and adjacent oilfields and a decrease in exploration by major oil companies. This project will provide information that will encourage exploration in an underexplored part of northern Alaska that includes the National Petroleum Reserve-Alaska, State lands, and Native Corporation lands. The project will also help encourage exploration in northern Alaska by smaller independent oil companies by providing public access to much-needed data and exploration concepts in this geologically complex region.
Understanding the evolution of fractures in the Colville basin hydrocarbon system is critical to developing a better working model of the hydrocarbon potential of the region. Naturally occurring fractures can play a key role in the evolution and producibility of a hydrocarbon accumulation. Fractures can both provide pathways for hydrocarbon migration into a reservoir and enhance permeability within a reservoir. Fractures are dynamic and sensitive to in situ pressure and can be damaged or destroyed during drilling and production.
Fractures develop at different times during the evolution of a hydrocarbon system, under a variety of conditions and due to a variety of causes. It is common for fracture formation to be intimately related to the structural history of the host rocks and difficult to predict. In this project, researchers will study the distribution, conditions, and timing of fracture formation in the Colville basin and adjacent Brooks Range foothills of northern Alaska, with a focus on the timing of fracture formation relative to trap formation and hydrocarbon generation and migration.
The project consists of three major tasks. Two regional transects across the eastern and central Brooks Range foothills and adjacent Colville basin will be constructed using new and available detailed geologic surface and subsurface mapping, new geochronologic and thermal data, and existing regional structural, thermal, and geochronologic information. These data will be used to develop retrodeformable balanced cross sections that will provide a model of when, where, and at what depth critical fractures formed.
Concurrently with the detailed field studies, subsurface well data from the Colville basin will be used to develop a regional model of the present day in-situ stress distribution within the basin. In-situ stresses control the type and orientation of fractures and the depth at which they occur. Integrating the current day in-situ stress distribution with the known fracture patterns should provide a regional picture of the depth and orientation of the open fracture networks and thus the orientation of basin-scale fluid flow at any one time within the basin.
Current Status (March 2007)
The project is in the beginning of its fourth year. All three phases of the project are nearing completion. The project was scheduled to be completed by September 1, 2006, but the completion date has been extended for 12 months to August 31, 2007.
This project was selected in response to DOE’s Arctic Energy Office solicitation DE-FC26-01NT41248.
Project Start: September 1, 2004
Project End: August 30, 2007
Anticipated DOE Contribution: $458,000
Performer Contribution: $132,000 (22 percent of total)
NETL - James Hemsath (firstname.lastname@example.org or 907-452-2672)
U. of Alaska Fairbanks – Catherine Hanks (email@example.com or 907-474-5562)
Results of this project have been presented as papers at national meetings, including those of the American Association of Petroleum Geologists and the Geological Society of America.
The Trans-Alaska Pipeline is shown against the backdrop of the Brooks Range foothills.