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Record W2318072106 · doi:10.1190/sbgf2011-255

Near-surface S-wave velocity models from two uphole surveys

2011· article· en· W2318072106 on OpenAlexaffabout
Saúl E. Guevara, Gary F. Margravé, William Agudelo, Fausto Gómez

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicSeismic Waves and Analysis
Canadian institutionsUniversity of Calgary
FundersEcopetrol
KeywordsSurface waveSurface (topology)GeologyComputer sciencePhysicsOpticsGeometryMathematics

Abstract

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PreviousNext No Access12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011Near-surface S-wave velocity models from two uphole surveysAuthors: Saul Guevara*Gary MargraveWilliam AgudeloFausto GomezSaul Guevara*CREWES-University of Calgary, Gary MargraveCREWES-University of Calgary, William AgudeloEcopetrol-ICP, and Fausto GomezEcopetrol-ICPhttps://doi.org/10.1190/sbgf2011-255 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InReddit Abstract Two uphole surveys were carried out at the location of an on-shore 3C survey in Colombia. An S-wave velocity model was obtained from these data, based on events apparently generated by the source. High variations in the velocity model with depth were observed and related to lithological characteristics. These variations can hardly be observed using surface seismic data. This velocity model can be useful in the computation of statics correction in the processing of converted-wave (PS) or S-wave seismic data, as well as in engineering and other near surface applications. Keywords: multicomponent, near surface, velocityPermalink: https://doi.org/10.1190/sbgf2011-255FiguresReferencesRelatedDetailsCited byMethod of building three-dimensional near-surface S-wave velocity model via down-hole surveysMin Li, Miaoyu Chen, Xiaoyang Wang, Zhichao Yang, Jiangli Chen, Pandeng Liu, Xiao Fan, Chenyi Li, and Yuefeng Sun27 August 2018Low velocity layer characterization in the Niger Delta: Implications for seismic reflection data quality2 September 2017 | Journal of the Geological Society of India, Vol. 90, No. 2Near-surface S-wave velocity from an uphole experiment using explosive sourcesSaul E. Guevara, Gary F. Margrave, and William M. Agudelo19 August 2013Using converted-wave seismic data for lithology discrimination in a complex fluvial setting: Tenerife oil field, Middle Magdalena Valley, ColombiaWilliam Agudelo, Edgar Pineda, Ricardo Gómez, Jairo Guerrero, Nelson Rojas, Rob Stewart, and Norbert van de Coevering31 December 2012 | The Leading Edge, Vol. 32, No. 1Seismic lithology discrimination in complex fluvial stratigraphy: Tenerife 3D 3C Survey, Middle Magdalena Valley (Colombia).William Agudelo, Ricardo Gómez, Jairo Guerrero, Ingrid Tatiana Cabrejo, Nelson Rojas, S.A Ecopetrol, and Saul Guevara25 October 2012 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011ISSN (online):2159-6832Copyright: 2011 Pages: 2223 publication data© 2011 Published in electronic format with permission by the Brazilian Geophysical SocietyPublisher:Society of Exploration Geophysicists HistoryPublished Online: 13 Mar 2014 CITATION INFORMATION Saul Guevara*, Gary Margrave, William Agudelo, and Fausto Gomez, (2011), "Near-surface S-wave velocity models from two uphole surveys," SEG Global Meeting Abstracts : 1237-1240. https://doi.org/10.1190/sbgf2011-255 Plain-Language Summary Keywordsmulticomponentnear surfacevelocityPDF DownloadLoading ...

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 score0.579
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)0.0250.001

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 head0.075
GPT teacher head0.211
Teacher spread0.136 · 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

Citations8
Published2011
Admission routes2
Has abstractyes

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