Geology of eastern Prince of Wales Island and adjacent smaller islands, Nunavut
Bibliographic record
Abstract
The report area forms a narrow, north-oriented rectangle in the south-central part of the Arctic Islands. The area comprises the northeastern part of Prince ofWales Island and adjacent smaller islands. The western part of the area is underlain by very gently dipping lower Paleozoic formations of the Arctic Platform, and the eastern part by Proterozoic sedimentary rocks and intrusions and by Archean crystalline rocks of the Boothia Uplift. A major, west-directed thrust zone separates the two areas. The Precambrian rocks comprise three assemblages: an Archean and/or lower Proterozoic basement of granulite grade metamorphic rocks (predominantly orthogneiss), its Mesoproterozoic cover of sedimentary rocks, and two suites of mafic igneous rocks of Meso- and Neoproterozoic ages. The Cambrian to mid-Silurian succession consists of minor sandstone and varied carbonate units. Upper Silurian and Lower Devonian rocks contain a large amount of terrigenous material in the vicinity of the Boothia Uplift, but they consist of carbonate deposits in the platform region. The north-trending gneissic fabric of the basement controlled the overall form of the Boothia Uplift. The basement is cut by northwest-, west-, and northeast-trending faults and fractures, which influenced its subdivision into numerous small blocks that acted semi-independently of one another. As a result, the western frontal fold and thrust belt of the Boothia Uplift, although continuous for 500 km and with consistent west-verging geometry, is remarkably heterogeneous in detail. Blocks with their own consistent geometry rarely exceed 10 km in strike length; a few are as small as 2 km long.
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 imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.002 | 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 teacher head, 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".