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Record W171265321

Structural controls on the seismic sequence stratigraphy of the Ben Nevis, Avalon, and Eastern Shoals formations, Terra Nova field, Jeanne D'Arc Basin, offshore Newfoundland

2003· dissertation· en· W171265321 on OpenAlexfundaboutno aff
Alison Gollop

Bibliographic record

VenueMemorial University Research Repository (Memorial University) · 2003
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsGeologyUnconformityShoalGrowth faultFault (geology)Fault blockCretaceousPaleontologyExtensional faultAptianSequence stratigraphySedimentary rockStructural basinSeismologyGeomorphologyRiftSedimentary depositional environment
DOInot available

Abstract

fetched live from OpenAlex

The structural controls on the seismic sequence stratigraphy of the lower Cretaceous succession in the Terra Nova oil field, Grand Banks of Newfoundland, is studied using a digital 3-D seismic database and wireline log data from 11 offshore wells. Three seismic sequences (Units A, B, and C) were mapped in the Terra Nova area, roughly corresponding to the Eastern Shoals, Avalon, and Ben Nevis formations, respectively. Each sequence is bounded by distinct unconformities. The development of these sequences and their boundaries was controlled by an interplay of sediment input, changes in sea level, tectonism, accommodation space, and climate. However, tectonism (i.e., fault-block subsidence and rotation) is interpreted to be the principal cause for the sedimentary patterns and development of the major unconformities in the Terra Nova field; global eustatic sea-level variations had only a minor influence on unconformity generation. -- The N-S-trending fault system in the Terra Nova field was active during the Tithonian to mid-Valanginian, as evidenced by fault growth within the Hibernia and Rankin formations. The E-W-trending fault system was previously interpreted to have been formed during mid-Aptian to Albian extensional phases; however, growth-strata patterns within the Eastern Shoals Formation suggest instead that the E-W-trending fault system in the Terra Nova field was initiated by at least the late Barremian and was active until late Albian. Also, the N-S-trending fault system in the Terra Nova field was reactivated at this time. This fault system terminates upward against the Albian unconformity, so that by late Albian the active rifting in the Terra Nova field is interpreted to have ceased. -- A "pop-up" feature immediately west of the Voyager Fault in the Terra Nova field has been previously interpreted to have formed by transpressional stresses induced by oblique-slip movement. However, geometries similar to those presented in the model of Jackson and Vendeville (1992 and 1994) suggest that a large salt diapir may lie in the footwall of the Voyager Fault. Therefore, an alternative interpretation is proposed for this "pop-up" feature, as a localized contractional feature related to diapirism. -- The lower Cretaceous succession in the Terra Nova field does not contain hydrocarbons, but forms reservoirs in other oil fields such as Hibernia and White Rose. It is proposed that the reservoir facies represented by the Ben Nevis and Avalon formations in the Terra Nova field were charged with hydrocarbons at some point but were subsequently breached, allowing oil to escape from the traps. This scenario is consistent with published fluid-inclusion studies.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.304
Threshold uncertainty score0.612

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.001
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.030
GPT teacher head0.235
Teacher spread0.205 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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
Published2003
Admission routes2
Has abstractyes

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