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Record W3016721852 · doi:10.1130/abs/2020se-344176

THE MOUNT EPHRAIM BLOCK, COBEQUID HIGHLANDS, NOVA SCOTIA, CANADA: A SIGNIFICANT CA. 750-735 MA MAGMATIC ARC EVENT IN AVALONIA

2020· article· en· W3016721852 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueAbstracts with programs - Geological Society of America · 2020
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicArchaeology and ancient environmental studies
Canadian institutionsnot available
Fundersnot available
KeywordsMountNova scotiaNova (rocket)GeologyBlock (permutation group theory)Event (particle physics)Arc (geometry)Back-arc basinSeismologyComputer sciencePhysicsSubductionAstrophysicsTectonicsAeronauticsOceanographyOperating systemEngineering

Abstract

fetched live from OpenAlex

The fault-bounded Mount Ephraim block forms the eastern part of the Avalonian Cobequid Highlands of northern mainland Nova Scotia. Mapping, petrological work, and new U-Pb zircon dating have shown that the block includes ca. 800 Ma quartzofeldspathic, semi-pelitic, and pelitic gneiss and schist of the Mount Thom Formation, ca. 750 Ma volcanic rocks of the Dalhousie Mountain Formation, 780(?) to 730 Ma gabbroic/dioritic to granitic plutons of the Mount Ephraim suite, and ca. 740-730 Ma dioritic rocks of the Six Mile Brook pluton. The plutonic rocks are magnesian and calc-alkalic and formed in a continental margin subduction zone. Eight samples from the Mount Ephraim suite have epsilon Nd ranging from -1.7 (monzogranite) to +1.7 (gabbro). These older units are intruded by the ca. 635 Ma calc-alkalic arc-related granodioritic Gunshot Brook Pluton (epsilon Nd 0.5 and 0.6). An elongate body of within-plate syenite to alkali-feldspar granite and gabbro intruded the Mount Thom Formation and Mount Ephraim suite along their southern margin yielded zircon ages of 482–480 Ma indicating a link to similar alkalic rocks in the Antigonish Highlands by the Ordovician. The Mount Ephraim block contrasts with other components of the Cobequid Highlands in the Bass River and Jeffers blocks. The Bass River block along the southernmost margin of the highlands consists of mafic metavolcanic rocks interbedded with quartzite, metawacke, and minor marble and ironstone of the Folly River and Gamble Brook formations, with maximum depositional ages of ca. 1 Ga. These units are intruded by abundant ca. 622 and ca. 610 Ma calc-alkalic arc-related plutonic rocks. The Rockland Brook mylonite zone separates the Bass River block from ca. 625 to ca. 590 Ma volcanic rocks and co-magmatic calc-alkaline granitoid rocks of the Jeffers block, considered typical of Avalonia. However, a U-Pb zircon age of ca. 745 Ma from rhyolite porphyry in the Jeffers block may indicate a link between the Jeffers and Mount Ephraim blocks. Although similar in age to the Mount Ephraim rocks, the Burin Group in the Newfoundland consists of pillowed basalt and other mainly mafic rocks interpreted to have formed in an ensimatic arc. The magmatic events recorded in the Mount Ephraim block provide potential sources for Cryogenian and Tonian inherited/detrital zircon elsewhere in Avalonia.

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.

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 score0.110
Threshold uncertainty score0.728

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 studies0.0000.002
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 head0.014
GPT teacher head0.201
Teacher spread0.186 · 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