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Record W4412735071 · doi:10.3749/2400035

Overview of Brine-Hosted Lithium Mineral Resources, Distribution, and Genesis in the Western Canada Sedimentary Basin

2025· article· en· W4412735071 on OpenAlexaffabout
Brendan Bishop, Leslie J. Robbins

Bibliographic record

VenueThe Canadian Journal of Mineralogy and Petrology · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsUniversity of Regina
Fundersnot available
KeywordsGeochemistryGeologyBrineStructural basinSedimentary rockMineral resource classificationEarth scienceGeomorphologyChemistry

Abstract

fetched live from OpenAlex

Abstract Saline brines from sedimentary basins could play a key role in providing the Li required for the energy transition. In the Western Canada Sedimentary Basin, economic (>75 mg/L) Li concentrations have been discovered in brines of Late Devonian-aged strata, specifically the Leduc, Nisku, and Swan Hills formations of Alberta and the Duperow Formation of Saskatchewan. Through industry activity, 75.9 M tonnes Inferred, 14.9 M tonnes Indicated, and 7.2 M tonnes Measured Li carbonate equivalent mineral resources, and Probable and Proven mineral reserves of 997,000 tonnes LCE and 141,000 tonnes LCE, respectively, have been identified. However, much of the exploration has primarily relied on historical brine data. Therefore, other prospective Li targets may have yet to be discovered, requiring the development of a deposit model to guide exploration to new areas. A key requirement for developing such a model is identifying the Li source. This work surveys the occurrences and distribution of Li in the Western Canada Sedimentary Basin, provides a compilation of the first Li-brine database and mineral resource estimates, discusses the implications for shared pore space policy, and examines hypotheses for the Li source. Seawater evaporation, evaporite dissolution, and contributions from the Precambrian basement have each been proposed as key factors in generating Li-rich brines in the Western Canada Sedimentary Basin, however, based on geochemical and isotopic evidence, as well as findings from other basins, we advocate for water–rock interactions with Li-rich shales. Other factors, such as dolomitization, clay transformations, evaporation, lithology, and the depositional environment, may also play a role. Understanding the genesis of Li-rich brines and developing a deposit model is crucial for guiding future exploration in sedimentary basins. A key issue for new pore space users in sedimentary basins, which includes lithium, helium, geothermal energy, and carbon sequestration, is sharing of the pore space. Issues may arise as competition for pore space grows, especially in areas where activities can overlap, necessitating that the development of established and emerging resources be guided by informed policy to ensure all stakeholders benefit. Basinal brine-hosted Li has the potential to be a significant new source of Li on a global scale and provide a greener source of a critical metal required for the energy transition, with western Canada well positioned to play an important role in this emerging field.

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)0.001
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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.075
Threshold uncertainty score0.149

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
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 head0.017
GPT teacher head0.205
Teacher spread0.188 · 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 designObservational
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

Citations2
Published2025
Admission routes2
Has abstractyes

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