MétaCan
Menu
Back to cohort
Record W2291323780

Abstract: Possible applications for visible/infrared reflectance spectroscopy (VIRS) in exploration for rare-earth elements

2011· article· en· W2291323780 on OpenAlexvenueaboutno aff
Heather Rafuse, Andrew Andrew

Bibliographic record

VenueAtlantic Geology · 2011
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsMonaziteHydrothermal circulationRare-earth elementMineralization (soil science)GeologyMineralogySpectroscopyAbsorption (acoustics)Infrared spectroscopyGeochemistryRare earthChemistryMaterials scienceSoil sciencePaleontologyZircon
DOInot available

Abstract

fetched live from OpenAlex

Visible-Infrared Reflectance Spectroscopy (VIRS) uses absorption responses to electromagnetic radiation of 350–2500 nm wavelengths to characterize natural materials and identify minerals that have distinct absorption spectra. Its principal application in exploration geoscience is in the study of hydrothermal alteration assemblages, but the current interest in exploration for rare-earth element (REE) deposits awakened our interest in possible applications to this type of mineralization. Some interesting possibilities emerged from pilot studies. Individual REE oxides have unusual absorption responses in the visible region (390 nm–750 nm) and notably in the near infrared (NIR; 750 nm to 1300 nm), which is normally a relatively “quiet” region for natural minerals. REE-bearing minerals (e.g., monazite, bastnaesite, betafite and xenotime) also produce these unusual NIR absorption features. This behaviour is related to the unique electron shell configurations of the lanthanide elements, and the absorption patterns are highly specific. However, there are presently few spectra from REEbearing minerals in the available reference databases, and such minerals typically show wide variations in composition, including REE distributions. Notwithstanding these complications, VIRS data acquired from mineralized samples in several areas of Labrador reveal distinctive spectral responses indicative of REE, even though their exact mineralogical sources are not yet readily identifiable. This implies that VIRS analysis could be used to test for potential REE mineralization in samples identified on the basis of other criteria such as anomalous radioactivity. However, the threshold for such detection is as yet unknown. The diverse styles of REE mineralization now identified in Labrador afford us an opportunity to gather and distribute VIRS absorption spectra for unusual minerals, which may be useful to explorationists elsewhere. As an example, the first reference spectra for the Na-Ca-Fe-Zr-REE silicate eudialyte (from the Red Wine Mountains area) are presented and discussed. The VIRS method may also be of use as a first-order tool for recognizing favourable host rocks to REE mineralization. This type of mineralization is commonly associated with peralkaline igneous suites. Peralkalinity is a geochemical characteristic that can be discerned through whole-rock analyses,

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 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: Theoretical or conceptual · Consensus signal: Theoretical or conceptual
GenreCandidate signal: Methods · Consensus signal: none
Teacher disagreement score0.794
Threshold uncertainty score0.613

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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
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 head0.040
GPT teacher head0.280
Teacher spread0.240 · 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 teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designTheoretical or conceptual
Domainnot available
GenreMethods

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
Published2011
Admission routes2
Has abstractyes

Explore more

Same venueAtlantic GeologySame topicGeochemistry and Geologic MappingFrench-language works237,207