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Record W7020065876

Isotopic and petrologic constraints on intracontinental deformation and metamorphism, Churchill Province, Nunavut

2024· dissertation· en· W7020065876 on OpenAlexaboutno aff

Bibliographic record

VenueMspace (University of Manitoba) · 2024
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsMetamorphismArcheanGeochronologyShear zoneMetamorphic rockTectonicsDeformation (meteorology)Shear (geology)Alpine orogeny
DOInot available

Abstract

fetched live from OpenAlex

The Canadian Churchill Province was the locus of repeated, regional reworking in the Paleoproterozoic associated with five major orogenic events that ultimately resulted in the formation of Earth’s first supercontinent, Nuna. Tectonic models for the Archean and Paleoproterozoic evolution of the Churchill Province have been formulated at the broadest scale, and consequently, the timing, nature and regional extent of deformation and metamorphism associated with these collisional events are poorly constrained. In this thesis, the metamorphic and deformation histories of two relatively unexplored regions in Nunavut were characterized in order to contribute to the understanding of the processes that reworked the boundaries and interior of the Churchill Province during development of Nuna. Aeromagnetic data and geological mapping on Boothia Peninsula, Nunavut, revealed the presence of a ~165 km long, 5-10 km wide high-strain zone, named the Sanagak Lake shear zone (SLsz), that marks the transition from dominantly N-trending Thelon-related structures in the north to SW-trending Trans-Hudson-related structures in the south. Field, microstructural, petrologic and isotopic data indicated that the SLsz is a south-dipping, strike-slip (sinistral) shear zone that formed in the mid-crust (~ 0.52 GPa) at 1804 ± 6 Ma. The timing, geometry and kinematics of high-strain deformation is consistent with north-directed compression associated with far-field stresses derived from the Trans-Hudson orogeny, and marks the northern limit of Trans-Hudson related deformation. Geologic mapping, phase equilibria modelling, and multi-mineral geochronology coupled with previously collected petrological and isotopic data from the Baker Lake area outline four lithotectonic domains named the Woodburn Lake and Ketyet River groups, Quoich River domain, Kramanituar Complex and the Thirty Mile domain. Each of these domains experienced distinct pressure – temperature – time – deformation (P-T-t-d) histories and are separated by shear zones that facilitated differential burial-exhumation in the Paleoproterozoic. All domains were buried and reworked, to varying degrees, between ca. 1.93 and 1.90 Ga during the Snowbird Orogeny. The Kramanituar Complex was exhumed rapidly following ca. 1.9 Ga metamorphism, whereas the Quoich River and Thirty Mile domains exhumed between ca. 1.87 and 1.85 Ga during the accretionary phases of the Trans-Hudson Orogeny.

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 score0.015
Threshold uncertainty score0.092

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0030.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.010
GPT teacher head0.172
Teacher spread0.162 · 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
Published2024
Admission routes1
Has abstractyes

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