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Record W2321171397 · doi:10.1190/1.3063763

3‐D Magnetic data‐space inversion with sparseness constraints

2008· article· en· W2321171397 on OpenAlexaff
Mark Pilkington

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeophysical and Geoelectrical Methods
Canadian institutionsGeological Survey of Canada
Fundersnot available
KeywordsInversion (geology)Computer scienceSpace (punctuation)GeologySeismology

Abstract

fetched live from OpenAlex

An inversion approach is presented that determines the three‐dimensional (3D) susceptibility distribution that produces a given magnetic anomaly. The subsurface model comprises a 3D, equally‐spaced array of dipoles. The inversion incorporates a model norm that enforces sparseness and depth‐weighting of the solution. Sparseness is imposed by using the Cauchy norm on the model parameters. This constrains the resulting model to be simple, with no excessive structure. The inverse problem is posed in the data space, leading to a linear system of equations with dimensions based on the number of data, N. This contrasts the standard least squares solution, derived through operations within the M‐dimensional model space (M being the number of model parameters). Hence, the data‐space method leads to computational efficiency by dealing with an N×N system versus an M×M one, where N≪M. Inversion of aeromagnetic data collected over a Precambrian Shield area shows that including the sparseness constraint leads to a simpler and better resolved solution

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 imitation

Not 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.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.804
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.001

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 head0.042
GPT teacher head0.228
Teacher spread0.185 · 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; both teacher heads agree on what is shown here.

Study designObservational
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

Citations12
Published2008
Admission routes1
Has abstractyes

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