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Record W2966064025 · doi:10.1306/1025703h13127

Structural Style and Hydrocarbon Potential in the Acadian Foreland Thrust and Fold Belt, Gaspé Appalachians, Canada

2004· article· en· W2966064025 on OpenAlexaffabout
D. Kirkwood, Martin Lavoie, J. S. Marcil

Bibliographic record

VenueAmerican Association of Petroleum Geologists eBooks · 2004
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsOnex (Canada)Université Laval
Fundersnot available
KeywordsGeologyForeland basinDevonianFold (higher-order function)OrogenyFold and thrust beltPaleontologyOrdovicianPaleozoicTectonicsTranspressionHydrocarbon explorationSeismologyShear zone

Abstract

fetched live from OpenAlex

Abstract For more than 150 yr, the Gaspé Peninsula in the northern Appalachians has generated interest for oil and gas exploration. Although oil shows and seeps are abundant, oil production has been minor. The hydrocarbon potential is restricted to Late Ordovician to Early Devonian rocks of the Gaspé belt, and different play concepts have been explored over the years. The recent discovery of the Junex-Galt natural gas field has renewed interest for onshore hydrocarbon exploration in this area of eastern Canada. We propose a new structural model for the Middle Devonian Acadian orogeny involving development of an early foreland thrust and fold belt with deformation accommodated by folding, considerable tectonic wedging, blind north-verging thrusts, south-verging backthrusts, and a possible triangle zone followed by strike-slip faulting that partially dissected the thrust and fold belt. Previous interpretations of the tectonic evolution of the Gaspé belt during the Acadian orogeny was that of a tranpressional orogen basically characterized by folds and strike-slip faults compatible with a wrench tectonic model. Instead, new field work and seismic data that were acquired by the Ministère des Richesses Naturelles du Québec (2000–2001) and presented here suggest enough shortening during the initial compressive phase to produce south-verging folds and south-directed motion along north-dipping reverse faults. The fold and thrust belt structural style proposed in this chapter offers a promising geological setting for potential structural traps and new hydrocarbon plays in the entire Gaspé Peninsula. Highly fractured zones are expected in domal structures above important blind thrusts and at thrust tips in areas of fault-propagation folding. Hydrocarbon migration has been documented through fractures in the Upper Ordovician to Lower Devonian Gaspé belt succession at different stages of its tectonic history. Major anticlines in the northeastern part of the Connecticut Valley-Gaspé synclinorium, i.e., Mississippi, Bald Mountain, and Holland anticlines, could be fault propagation located above blind thrusts. The Junex-Galt natural gas field is a good example of such a tectonic setting. Gas is trapped in a folded and fractured Devonian limestone that is located between two regional strike-slip faults at a depth of about 2250 m (7400 ft). Geochemical analyses from recovered oils in the area indicate a Devonian as well as an Ordovician origin very similar to oils from western Newfoundland. A large Ordovician anticline, which was imaged on old and newly acquired seismic lines, underlie the Galt area and represent deeper plays located above blind thrusts deep within the Acadian fold and thrust belt.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.086
Threshold uncertainty score0.358

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 head0.003
GPT teacher head0.167
Teacher spread0.164 · 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.

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

Citations11
Published2004
Admission routes2
Has abstractyes

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