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Record W2770720593 · doi:10.1190/sbgf2017-324

Smooth velocity model from traveltime tomography of an offshore dense wide-angle profile in Nova Scotia: preliminary results

2017· article· en· W2770720593 on OpenAlexaffabout
Fábio André Perosi, M. R. Nedimović, Keith E. Louden, K. W. Helen Lau

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicSeismic Imaging and Inversion Techniques
Canadian institutionsDalhousie University
Fundersnot available
KeywordsNova scotiaGeologyTomographySubmarine pipelineNova (rocket)SeismologyComputed tomographyGeodesyPhysicsOpticsOceanographyEngineeringMedicineRadiologyAerospace engineering

Abstract

fetched live from OpenAlex

Understanding the mechanisms that generate rifted continental margins is important in several aspects: (1) scientific - how continents break apart; (2) geopolitical -delimitation of the territorial sea through the United Nations Convention on the Law of the Sea (UNCLOS, United Nations Convention on the Law of the Sea) and; (3) economic, de-risking of oil and gas exploration. The goal of the work proposed here is to prestack migrate in a joint fashion the OETR-2009 OBS and NovaSpan 2000 MCS data. To the best of our knowledge, this would be the first attempt to carry out this type of data analysis and we anticipate significant improvements in the imaging with this approach, in particular of the crystalline basement, crust and the Moho. In order to construct an accurate and detailed but smooth velocity model needed for joint prestack migration of the OBS and MCS data, we will first run a detailed tomographic inversion of the OETR profile. The proposed work will show how velocity modeling of detailed wide-angle refraction observations (such as the OETR profile) can significantly improve the definition of the lower (deep) sediment and basement geometries. We also hope that our results will have a major impact on the sighting of future 3D reflection surveys and exploration wells. The preliminary result of smooth velocity model shows: the depth of the Moho discontinuity is estimated to be ~33 km in the continental crust over a distance of ~60 km, rapidly rising to ~24 km at the distance of ~100 km and, gradually, rising to ~13 km at 280 km within the oceanic crustal domain, with the same depth extending until the end of the model. Between 10-80 km distance, a LVL– HVL–LVL (LVL=Low Velocity Layer, HVL=High Velocity Layer) sequence is observed. In the OCT, between 200-260 km distance, there is a section above the Moho which has a strong gradient and high velocity in compared to normal crust velocities.

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 machine prediction

Teacher imitation

Not 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.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.451
Threshold uncertainty score0.907

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0000.001
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0010.000

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.

Opus teacher head0.025
GPT teacher head0.243
Teacher spread0.218 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
Domainnot available
GenreEmpirical

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".

Quick stats

Citations0
Published2017
Admission routes2
Has abstractyes

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