Paleoproterozoic to Mesoproterozoic evolution of Yukon Territory, Canada
Bibliographic record
Abstract
The supercontinent Columbia existed from approximately 1.8 to 1.3 Ga. During this time, complex tectonic interactions occurred between northwestern Laurentia and Australia. This thesis concerns three geologic events on northwestern Laurentia. The first event is the development of a post-collisional sedimentary overlap assemblage at 1.6 Ga herein called the Wernecke-Ogilvie unlithified succession (WOUS). The second event is the formation of the Wernecke Breccia, a set of 1.60 Ga hydrothermal breccia zones. The third is the emplacement of the 1.38 Ga Hart River sills. The WOUS was a succession of sandstone and mudstone that was deposited after collision between Laurentia and Australia at ~1.6 Ga, and prior to the formation of the Wernecke Breccias at 1.60 Ga. The WOUS is contained as clasts within the Wernecke Breccia. On the basis of detrital zircon U-Pb ages, Lu-Hf model ages and neodymium isotope geochemistry, the WOUS is correlated to sedimentary units within the hydrothermal breccias of the Olympic Dam deposit on the Gawler Craton of Australia. The Wernecke Breccia occurs as zones that are metres to kilometres in size that are scattered over an area of 300 x 150 km. The breccia zones are post-orogenic and are hosted by the deformed and metamorphosed Wernecke Supergroup. The breccias formed from voluminous hydrothermal surges with a significant gaseous component. These surges vented, and overlying rock units foundered kilometres deep into the breccia zones. The Hart River sills extend from the eastern Ogilvie Mountains to the Wernecke Mountains. Individual sills are up to 200 km long and 500 m thick. The sills are mafic to intermediate, and tholeiitic. The sills are dated herein at 1382.15 ± 0.39 Ma and 1382.14 ± 0.36 Ma. The magma that formed the sills resulted from ~10% partial melting of spinel bearing mantle similar to a MORB source. Coeval and possibly related magmatism occurred farther south on Laurentia, and to the north on Siberia. These magmatic events occurred on a possible rift axis that extended along the western margin of Laurentia and may signify breakup of the supercontinent Columbia.
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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 | 0.004 |
| Science and technology studies | 0.003 | 0.001 |
| Scholarly communication | 0.002 | 0.000 |
| Open science | 0.000 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.005 | 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".