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Record W2170340412

Study of holocene landslide deposits by comparison of GPR, refraction seismic and electrical resistivity data

2004· article· en· W2170340412 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueInternational Conference on Grounds Penetrating Radar · 2004
Typearticle
Languageen
FieldEngineering
TopicGeophysical Methods and Applications
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsLandslideGeologyGround-penetrating radarSeismic refractionHoloceneSeismologyRefractionElectrical resistivity and conductivityGeomorphologyElectrical resistivity tomographyRadarPaleontology
DOInot available

Abstract

fetched live from OpenAlex

This paper integrates the results of a geophysical investigation of Holocene landslide events in the Cypress Hills, Canada. Ground penetrating radar (GPR), P-wave refraction seismic and electrical resistivity imaging were used to delineate the boundaries of the landslide masses. GPR provided information about the first meters of the subsurface. The seismic refraction survey complemented the datasets provided by GPR, giving results from greater depths. The electrical resistivity method, in principle the most indicated technique for such clay rich deposits, was used to provide a general structure of the upper 30 meters. Results from two locations provide an overall image of the structure and information about the vertical extent of the landslide. Two different interfaces, that probably mark the top :and the bottom of the landslide, are depicted. In connection with these boundaries, the thickness of the landslide deposits is estimated to increase roughly from 10-15 to more than 20 meters towards the toe of the landslide.

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.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.832
Threshold uncertainty score0.326

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)0.0000.000

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 head0.071
GPT teacher head0.353
Teacher spread0.283 · 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