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Record W2995720479

STRUCTURAL EVOLUTION OF THE TWELVE MILE BAY SHEAR ZONE, GRENVILLE PROVINCE, ONTARIO, CANADA

2019· article· en· W2995720479 on OpenAlexaboutno aff
Peter Regan

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsBayMileGeologyGeographyGeodesyOceanography
DOInot available

Abstract

fetched live from OpenAlex

Shear zones are tabular structures of higher strain and vorticity relative to the country rock. Shear zones appear globally, at all scales, and commonly link together to form complex anastomosing patterns. The processes by which shear zones nucleate, propagate, and form networks have been studied extensively, but predominately in isotropic materials. The Twelve Mile Bay shear zone, located in the ca. 1.0 Ga Grenville orogen in Ontario, Canada, is a shear zone system developed with anisotropic rocks of the interior Parry Sound domain (iPSD). Granulite facies layering of the southern margin of the iPSD is transposed by a series of increasingly connected amphibolite facies shear zones within a five kilometer wide zone of progressive deformation, preserving several stages of shear zone development, resulting in the regional-scale shear zone between the iPSD and the lower Go Home domain. Outcrops were digitally imaged using innovative aerial photography and open source software to create high-resolution georeferenced aerial photo mosaics of several islands. Photo mosaics enabled quantitative measurement of strain along shear zones and their geometries at various stages of shear zone development. Measurements show an increase in shear strain (γavg) proximal to the Twelve Mile Bay shear zone and reveal a bimodal distribution of extension directions, from NNE-SSW at the start of the zone of transposition, to E-W toward the Twelve Mile Bay shear zone where transposition is complete. Folds within wall rocks at several stages of transposition revealed that fold hinges originate in a steeply plunging orientation and are reoriented into the shallowly plunging, E-W oriented, regional extensional direction of the Twelve Mile Bay shear zone (~E-W). This study proposes a conceptual model for the main stages of transposition along the southern margin of the iPSD: i) brittle fracture-filled pegmatite dykes introduced hydrated planes of weakness; ii) initial dextral shear zone developed along pegmatites; iii) sinistral shearing at a high angle to dextral shear zones that amplified pre-exisiting dextral shear zones and introduced internal wall rock deformation; iv) folded wall rock blocks are increasingly deformed and rotated into the regional extensional direction causing shear zone widening, which led to an increasingly linked shear zone network; and, v) complete transposition of iPSD layering to the shear zone fabric with rare pods of iPSD fabric.

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 score0.042
Threshold uncertainty score0.307

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0040.001
Scholarly communication0.0020.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0060.001

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 head0.005
GPT teacher head0.153
Teacher spread0.148 · 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
Published2019
Admission routes1
Has abstractno

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