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Record W4411250903 · doi:10.1186/s40517-025-00352-7

Heat resource potential and reservoir characteristics of fractured and dolomitized carbonates of the Beaver River gas field, Liard Basin, western Canada

2025· article· en· W4411250903 on OpenAlexafffundabout
Zhuoheng Chen, Stephen E. Grasby, Makram Hedhli

Bibliographic record

VenueGeothermal Energy · 2025
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsGeological Survey of Canada
FundersOffice of Energy Research and DevelopmentNatural Resources Canada
KeywordsGeologyBeaverStructural basinNatural gas fieldResource (disambiguation)Hydrology (agriculture)Drainage basinGeochemistryGeomorphologyPaleontologyNatural gasGeotechnical engineeringGeographyComputer scienceChemistry

Abstract

fetched live from OpenAlex

Abstract Petroleum exploration and development in northern Canada revealed high-temperature resources with sustainable water flow rates in several dolomite-hosted gas reservoirs in the Manetoe facies, along the western margin of the Liard Basin that extends across NE British Columbia, SW Northwest Territories, and SE Yukon. This study examines the characteristics of fractured Manetoe dolomite reservoirs and evaluates the geothermal potential of the Beaver River gas field. The goal is to assess its viability for geothermal energy utilization to benefit northern communities. A volumetric method, coupled with a wellhead flow rate approach, was applied to estimate both heat resource potential and production capacity. In addition, a sensitivity analysis was conducted to identify key factors influencing heat production capacity. Our assessment indicates that the Beaver River gas field contains a recoverable heat energy resource of 1.9 × 10 11 MJ, with potential to generate more than 24 MW electricity for over 30 years. A single well in the field is estimated to have nearly 3 MW of gross electricity capacity. The sensitivity analysis identified flow rate as the most important factor for production capacity, highlighting the critical role of open fractures associated with faulting and folding from the Laramide Orogeny in enhancing reservoir permeability and deep-water circulation connecting to the Manetoe dolomite reservoir. A combination of hydrothermal dolomitization and post-diagenetic tectonic deformation makes the fractured Manetoe facies a unique reservoir/aquifer suitable for hosting both petroleum and geothermal resources. Furthermore, several large gas fields in the fractured Manetoe dolomite reservoir, along the same tectonic trend in the Liard Fold and Thrust Belt, share similar reservoir characteristics and production behavior, and may also contain substantial extractable geothermal resources. The detailed subsurface geology and production behaviors from those depleted natural gas fields can serve as analogs for geothermal exploration and wellsite selection in northern Canadian communities where reservoirs are not well characterized, such as the hamlet of Fort Liard, NWT. This study also provides valuable insights more generally for geothermal exploration within carbonate aquifers in deformed foreland basins. Highlights Large geothermal potential in Manetoe facies carbonates of the Liard Fold and Thrust Belt Reservoir characterized by dual porosity-permeability, high flow rate, and slow pressure decline Beaver River gas field is a good analog for carbonate geothermal aquifers in deformation belt Alternative drilling site proposed for heat extraction in hamlet of Fort Liard

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.240
Threshold uncertainty score0.991

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.003
GPT teacher head0.169
Teacher spread0.166 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes3
Has abstractyes

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