MétaCan
Menu
Back to cohort
Record W2311594764 · doi:10.14288/1.0052675

The Orpheus Graben, offshore Nova Scotia : palynology, organic geochemistry, maturation and time : temperature history

2010· article· en· W2311594764 on OpenAlexaboutno aff
Erik Lyngberg

Bibliographic record

VenuecIRcle (University of British Columbia) · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsNova scotiaGrabenGeologyPalynologySubmarine pipelineNova (rocket)GeochemistryPaleontologyOceanographyPollenTectonics

Abstract

fetched live from OpenAlex

Palynological biostratigraphy and maturation data are combined to reconstruct the burial and thermal history of the Orpheus Graben, offshore Nova Scotia. Palynological analysis indicated that, 1) the age of sediments in the Orpheus Graben range from Upper Triassic to Turonian (Upper Cretaceous) with unconformities occurring in two wells, 2) recycled palynomorphs are ubiquitous in the wells examined, but do not occur in large numbers, 3) the Jurassic section is dominated by Classopollis, indicating an arid environment. The Cretaceous section is dominated by Cyathidites, Taxodiaceapollinites, Gleicheniidites and bisaccate pollen indicating wet tropical or sub-tropical conditions. Maturation zones were determined primarily by spore colour and correlation to vitrinite reflectance and pyrolysis data. Thermally mature rocks occur as shallow as 500 m in one well. The Dawson Canyon and Logan Canyon Formations contain the riches oil prone source rock. Enhanced levels of maturity were found to occur over salt structures. Burial history diagrams are shown for all six wells drilled in the Orpheus Graben as well as burial diagrams for a basin cross section through time. Two models of Tertiary subsidence are considered, 1) with minimal Tertiary deposition, 2) with up to 2000 m of Tertiary deposition. The temperature history of each well drilled in the Orpheus Graben can be inferred by combining the Time-Temperature Index and maturation data. Two temperature distributions are considered, 1) a simple temperature history with geothermal gradients twice the present and up to 2000m of Tertiary deposition and, 2) a complex Temperature history with geothermal gradients up to six times the present with minimal Tertiary deposition. The complex temperature history yields Time-Temperature Index values that are closer to the observed maturity. The future exploration potential is discussed, with enhanced exploration objectives suggested for the region further eastward along the axis of the Orpheus Graben.

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)0.000
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 score0.203
Threshold uncertainty score0.408

Distilled classifier scores by category (both heads)

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

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 head0.004
GPT teacher head0.140
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; 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

Citations1
Published2010
Admission routes1
Has abstractyes

Explore more

Same venuecIRcle (University of British Columbia)Same topicGeological formations and processesFrench-language works237,207