Abstract: Sequence-stratigraphic interpretations of alluvial-lacustrine basins: Uinta Basin, Utah, as an analogue of the Moncton Basin, New Brunswick
Bibliographic record
Abstract
Sequence stratigraphy has proved to be a powerful itself is tilled and bypassed. approach to the modeling of stratal successions in increasingly The three-dimensional facies distributions developed at diverse types of sedimentary basins. However, only limited each stage are controlled by the long tenn climatic belt the work has yet been done in lacustrine basins. Models are of low basin was situated in. Both basins have lithofacies associations resolution, and case studies are rare. New data from the recent indicative of a wet to seasonally dry climate, the Moncton Shell Canada drilling program in the Mississippian of the Basin being the wetter (the Gautreau evaporite being very Moncton Basin will provide an opportunity to apply a localized). Wet climates maintain high lake levels and high sequence stratigraphy to the Albert and associated fonnations relief, highstand deltas, whereas more seasonal climates and to aid in the development of higher resolution models. Of produce highly fluctuating lake levels containing deltas with interest is how the succession might compare to the analogous low preserved relief, and some evaporites toward the basin Uinta Basin of Utah. · centre. Both basins have the typical five-part succession that Work in the Uinta Basin is further advanced and may spans the entire lifespan of intennontane lacustrine basins and indicate what the Moncton Basin study might reveal. A cyclic which reflects the general tectonic control over basin initiation climatic control and irregular tectonic control on higher and fill. Alluvial strata associated with basin initiation is frequency, low relief sequences has been identified in the followed by a sediment starved, Iacustrine dominated lower Green River Fonnation (Dawson Settlement Member succession where tectonism is deepening the basin faster than equivalent). An overriding climatic control influences the high sediment is infilling. Changing tectonic controls and, or, relief sequence of the Uinta Formation (Hiram Brook Member increased sediment supply causes sediment to accumulate as equivalent). deltaic and ultimately fluvial successions before the basin
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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 | 0.001 | 0.001 |
| Science and technology studies | 0.001 | 0.000 |
| Scholarly communication | 0.001 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.004 | 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".