New insights into the crustal structure of northern Baffin Bay
Bibliographic record
Abstract
The Baffin Bay, located between Canada and Greenland, is a sediment filled oceanic basin which developed during Paleocene and Eocene times. Its genesis is closely related to the opening of Labrador Sea and Davis Strait. While the crust of the Labrador Sea and Davis Strait has been studied in detail, data on central and northern Baffin Bay is scarce. Southern Baffin Bay is underlain by oceanic crust with volcanic margins. The margins of northern Baffin Bay are characterized by serpentinized mantle material. To study the crustal structure of central and northern Baffin Bay and analyse the change from amagmatic to volcanic margins, a multidisciplinary scientific cruise was undertaken in 2010. Refraction seismic profiles were acquired along with other geophysical data in the Greenlandic part of Baffin Bay. We present a P-wave velocity model of one of these profiles. The 321-km-long profile consists of 25 ocean bottom seismometers (OBS) and runs from the deep area of northern Baffin Bay to the shelf area of Melville Bay. \nThe model can be divided into different crustal sections: In the central Northern Baffin Bay, 6-km-thick sediments overlay a 3-5 km thick oceanic crust, which thickens towards the continental slope. At the shelf edge, a buried seamount and high velocities in the lower crust are indicators for volcanic activity and intrusions of mafic material in this region. These features mark the onset of the transition between oceanic and continental crust. The stretched continental crust of Melville Bay is characterized by basement highs and deep sediment basins. Well constrained reflections of the Moho can be found at a depth of 22-24 km in many seismic sections. Near the Greenland margin, a basement outcrop, characterized by high velocities, is present.
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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 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.002 |
| Science and technology studies | 0.001 | 0.001 |
| Scholarly communication | 0.001 | 0.001 |
| Open science | 0.000 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.003 | 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".