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Record W3190198768

Stratigraphic analysis of the Scan Basin (south Scotia Sea, Antarctica): palaeoceanographic implications

2012· article· en· W3190198768 on OpenAlexaboutno aff
Lara F. Pérez, Francisco Javier Hernández Molina, Andrés Maldonado López, F.J. Lobo

Bibliographic record

VenueGeotemas ( Madrid ) · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Tectonic Studies in Latin America
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyCircumpolar starOceanographyNova scotiaStructural basinPaleontologyGeographyHumanities
DOInot available

Abstract

fetched live from OpenAlex

espanolLa parte sur del Mar de Scotia (Antartida) es clave para la reconstruccion de la circulacion oceanica profunda relacionada con las masas de agua que fluyen a traves de la Dorsal Meridional de Scotia. Desde el Mioceno Medio se han desarrollado pequenas cuencas oceanicas que han modificado la disposicion de los portales oceanicos profundos que permiten el flujo del Agua Profunda Circumpolar (CDW) y el Agua Profunda del Mar de Weddell (WSDW). La mas oriental es la Cuenca Scan, situada al norte de la Dorsal Meridional de Scotia y limitada al oeste y al este por los bancos Bruce y Discovery respectivamente. Durante las campanas oceanograficas SCAN1997 y SCAN2004 a bordo del BIO Hesperides, se obtuvieron siete perfiles de sismica de reflexion multicanal cuyo analisis ha permitido definir el patron estratigrafico y la evolucion morfoestructural de la cuenca. En el registro sedimentario se han identificado cuatro grupos de unidades: Basal, Inferior, Medio y Superior. El Grupo Basal esta formado por unidades sedimentarias antiguas deformadas, mientras los tres grupos superiores presentan facies sismicas mas similares. Las discontinuidades que limitan estas unidades estan relacionadas con eventos tectonicos y paleoceanograficos que han tenido lugar desde el Mioceno hasta la actualidad. EnglishThe southern part of the Scotia Sea (Antarctica) is a key area for the deep-water circulation reconstruction across the South Scotia Ridge. Several small oceanic basins were developed in this area since the Middle Miocene, and their evolution have influenced the Circumpolar Deep Water (CDW) and the Weddell Sea Deep Water (WSDW) circulation. The eastern most of these basins is the Scan Basin, located northwards of the South Scotia Ridge and the Jane Basin. It is bound to the west and to the east by the Bruce and Discovery banks respectively. Seven Multichannel Seismic profiles (MCS) were obtained during the SCAN1997 and SCAN2004 oceanographic cruises onboard the BIO Hesperides. The seismic analysis of those profiles reveals the stratigraphic pattern and the morphostructural evolution of the Scan Basin. Four major seismic unit-packages are identified within the sedimentary record, called from bottom to top: Basal, Lower, Middle and Upper. The Basal Package consists of deformed depositional units, whereas the three upper packages exhibit similar seismic facies. The discontinuities bounding those seismic units are linked to major tectonic and palaeoceanographic events since the Miocene to the present.

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 categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.020
Threshold uncertainty score0.995

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.003
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0060.000

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 head0.016
GPT teacher head0.216
Teacher spread0.201 · 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 teacher head, not a consensus.

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

Citations0
Published2012
Admission routes1
Has abstractyes

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