MétaCan
Menu
Back to cohort
Record W2504124914

Short-lived mantle generated magmatic events and their dyke swarms: The key unlocking Earth's paleogeographic record back to 2.6 Ga

2006· article· en· W2504124914 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

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyCrustRiftPaleontologyVolcanoMantle (geology)Continental crustTectonics
DOInot available

Abstract

fetched live from OpenAlex

The continents preserve a rich record of short-lived mantle-generated magmatic events through time and space. Many of these events can now be dated routinely and precisely, with a resolution of a couple of million years or better. The spatial and temporal association of such events with rifting and continental break-up leads to remnants being preserved on originally adjacent (conjugate) margins and their respective hinterlands. Originally adjacent but now distant pieces of crust are thus likely to share remnants of one, if not several, short-lived magmatic events. The overall record of short-lived magmatic events (“magma bursts”) in a particular fragment of continental crust defines, in essence, a high-resolution “barcode” that characterizes the ancestry of that piece of crust. Originally adjacent pieces of crust (“nearest neighbours”) are thus likely to share part of their barcodes. Even though break-up margins may be severely modified and reworked during subsequent events, and many of the break-up related volcanic rocks may have long been eroded, associated dyke swarms have high preservation potential and are likely to preserve within them the high-resolution spatial and temporal information needed to allow successful paleogeographic reconstructions. Other independent, but generally more fuzzy data can then be used to test specific reconstructions based on the precise “piercing points” provided by coeval dyke swarms. In this paper we illustrate the general methodology and propose a new and detailed Superior-Hearne-Karelia reconstruction forming the core of 2.7-2.1 Ga supercraton Superia. In general, a complete characterization of all fragments of continental crust in terms of their magmatic event barcodes would be the most efficient way to solve Earth’s pre-Pangaea paleogeographic evolution, as far back as 2.6 Ga. High-resolution ages are the most efficient early filter to focus further work (e.g. paleomagnetism, geochemistry) on globally significant events. Only several hundred new ages would be required to catalyze a quantum leap of progress in this overall field. To store and efficiently disseminate all relevant data on short-lived magmatic events, we urgently need a peer-reviewed global database, similar to other formal databases in related fields that deal with globally significant datasets. To stimulate the creation of such an international database we herein propose datasheets that list the kind of information required for each short-lived magmatic event. Corresponding author: Wouter Bleeker Geological Survey of Canada 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8 Email: wbleeker@nrcan.gc.ca; tel: +1-613-995-7277

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.021
Threshold uncertainty score0.994

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0110.001

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 head0.016
GPT teacher head0.185
Teacher spread0.169 · 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

Quick stats

Citations212
Published2006
Admission routes1
Has abstractyes

Explore more

Same topicGeological and Geochemical AnalysisFrench-language works237,207