Depositional History and Petroleum Potential of the Middle Devonian Fort Vermilion Formation, Alberta
Bibliographic record
Abstract
The Devonian Fort Vermilion Formation in the Swan Hills area of Alberta comprises interbedded anhydrite and carbonates. Generally interpreted as being formed subaerially in a sabkha environment, a new depositional model is proposed for this unit whereby sedimentation occurred subaqueous in a protected, variably deep, restricted basin. Based upon core examination, petrography, and various geochemical analyses, four facies assemblages representing four environments were identified: restricted and hypersaline, early diagenetic, moderately restricted, and euhaline. Three models, differing primarily on scale and proximity to the marine environment are discussed; these are: i) salina; ii) restricted lagoon; and iii) lake. The evidence garnered through this study are most consistent with deposition in a hypersaline lagoon setting, cut off from the open marine environment. Early deposition was most restricted with fluctuating water chemistry resulting in the deposition of carbonate and evaporite units. Seawater and associated ions were supplied to the system via evaporative drawdown through a seaward barrier or tidal channels. Relative sea level rise resulted in a better connection with the open ocean and the end of evaporite deposition, though salinity-restricted conditions persisted, as demonstrated by a paucity of marine biota. Following further sea level rise normal marine conditions ensued. The petroleum potential of the Fort Vermilion Formation was also investigated, though it was determined that the absence of organic matter (indicated by very low TOC values) prevented the generation of any substantial amount of hydrocarbons.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.002 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.001 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.001 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".