Seismic Ambient Noise Characterization of a New Permanent Broadband Ocean Bottom Seismometer Site offshore Catalonia (Northeastern Iberian Peninsula)
Bibliographic record
Abstract
Research Article| September 01, 2010 Seismic Ambient Noise Characterization of a New Permanent Broadband Ocean Bottom Seismometer Site offshore Catalonia (Northeastern Iberian Peninsula) Tànit Frontera; Tànit Frontera Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) 1Institut Geològic de Catalunya, Barcelona, Spain Search for other works by this author on: GSW Google Scholar Arantza Ugalde; Arantza Ugalde Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) 2Observatori de l'Ebre, CSIC–URL, Horta Alta, 38, 43520 Roquetes, Tarragona, Spain Search for other works by this author on: GSW Google Scholar Carme Olivera; Carme Olivera Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) 1Institut Geològic de Catalunya, Barcelona, Spain Search for other works by this author on: GSW Google Scholar José Antonio Jara; José Antonio Jara Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) 3GEOCAT (Gestió de Projectes, S.A.), Barcelona, Spain Search for other works by this author on: GSW Google Scholar Xavier Goula Xavier Goula Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) 1Institut Geològic de Catalunya, Barcelona, Spain Search for other works by this author on: GSW Google Scholar Author and Article Information Tànit Frontera 1Institut Geològic de Catalunya, Barcelona, Spain Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) Arantza Ugalde 2Observatori de l'Ebre, CSIC–URL, Horta Alta, 38, 43520 Roquetes, Tarragona, Spain Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) Carme Olivera 1Institut Geològic de Catalunya, Barcelona, Spain Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) José Antonio Jara 3GEOCAT (Gestió de Projectes, S.A.), Barcelona, Spain Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) Xavier Goula 1Institut Geològic de Catalunya, Barcelona, Spain Institut Geològic de Catalunya c. Balmes, 209-211 08006 Barcelona, Spain augalde@igc.cat (A. U.) Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2010 by the Seismological Society of America Seismological Research Letters (2010) 81 (5): 740–749. https://doi.org/10.1785/gssrl.81.5.740 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation Tànit Frontera, Arantza Ugalde, Carme Olivera, José Antonio Jara, Xavier Goula; Seismic Ambient Noise Characterization of a New Permanent Broadband Ocean Bottom Seismometer Site offshore Catalonia (Northeastern Iberian Peninsula). Seismological Research Letters 2010;; 81 (5): 740–749. doi: https://doi.org/10.1785/gssrl.81.5.740 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search The scientific importance of long-term ocean-floor seismic observatories has been widely and internationally recognized by earth science communities. In addition to their usefulness in investigating global-scale geophysical processes, long-term ocean-floor observations are also required to better constrain regional tectonics. However, the implementation of ocean-floor seismic stations is a difficult task, and efforts have been made for more than two decades to resolve the technological and logistical issues associated with such deployments (Romanowicz et al. 2009; Suyehiro et al. 2006). Different programs in the United States and Canada (e.g., NEPTUNE Project, http://www.neptune.washington.edu), Japan (e.g.... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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 imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.001 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.001 |
| Science and technology studies | 0.000 | 0.001 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.001 | 0.000 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.002 | 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 teacher head, 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".