MétaCan
Menu
Back to cohort
Record W2035472244 · doi:10.2113/gsemg.17.1-2.67

Gold Mineralization at the Anomaly A Deposit, Clarence Stream Area, Southwestern New Brunswick: Distal Deposits of a Syn-Deformational Intrusion-Related Gold System?

2008· article· en· W2035472244 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.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
fundA Canadian funder is recorded on the work.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueExploration and Mining Geology · 2008
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsGeological Survey of CanadaUniversity of New Brunswick
FundersNatural Resources Canada
KeywordsGeological surveyIntrusionMineralization (soil science)GeologyArchaeologyGeochemistryGeographyPaleontology

Abstract

fetched live from OpenAlex

Research Article| January 01, 2008 Gold Mineralization at the Anomaly A Deposit, Clarence Stream Area, Southwestern New Brunswick: Distal Deposits of a Syn-Deformational Intrusion-Related Gold System? S. Watters; S. Watters 1New Brunswick Department of Natural Resources, Geological Surveys Branch, 207 Picadilly Road, P.O. Box 5040, Sussex, New Brunswick, E4E 5L2. *Present address: Geological Consultant 3262 Route 121, Apohaqui, New Brunswick, E5P 1B1. Search for other works by this author on: GSW Google Scholar S. Castonguay; S. Castonguay † 2Natural Resources Canada, Geological Survey of Canada—Québec division, rue de la Couronne, Québec, Québec, G1K 9A9. †Corresponding Author: E-mail: scastong@nrcan.gc.ca Search for other works by this author on: GSW Google Scholar G.G. Lutes; G.G. Lutes 3Geological Consultant, 87 Venus Crescent, Hanwell, New Brunswick, E3C 1N1. Search for other works by this author on: GSW Google Scholar M.J. McLeod M.J. McLeod 1New Brunswick Department of Natural Resources, Geological Surveys Branch, 207 Picadilly Road, P.O. Box 5040, Sussex, New Brunswick, E4E 5L2. Search for other works by this author on: GSW Google Scholar Author and Article Information S. Watters *Present address: Geological Consultant 3262 Route 121, Apohaqui, New Brunswick, E5P 1B1. 1New Brunswick Department of Natural Resources, Geological Surveys Branch, 207 Picadilly Road, P.O. Box 5040, Sussex, New Brunswick, E4E 5L2. S. Castonguay † 2Natural Resources Canada, Geological Survey of Canada—Québec division, rue de la Couronne, Québec, Québec, G1K 9A9. G.G. Lutes 3Geological Consultant, 87 Venus Crescent, Hanwell, New Brunswick, E3C 1N1. M.J. McLeod 1New Brunswick Department of Natural Resources, Geological Surveys Branch, 207 Picadilly Road, P.O. Box 5040, Sussex, New Brunswick, E4E 5L2. †Corresponding Author: E-mail: scastong@nrcan.gc.ca Publisher: Canadian Institute of Mining, Metallurgy and Petroleum Received: 22 Jan 2004 Accepted: 17 Jun 2006 First Online: 02 Mar 2017 © 2008 Canadian Institute of Mining, Metallurgy and Petroleum Exploration and Mining Geology (2008) 17 (1-2): 67–84. https://doi.org/10.2113/gsemg.17.1-2.67 Article history Received: 22 Jan 2004 Accepted: 17 Jun 2006 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation S. Watters, S. Castonguay, G.G. Lutes, M.J. McLeod; Gold Mineralization at the Anomaly A Deposit, Clarence Stream Area, Southwestern New Brunswick: Distal Deposits of a Syn-Deformational Intrusion-Related Gold System?. Exploration and Mining Geology 2008;; 17 (1-2): 67–84. doi: https://doi.org/10.2113/gsemg.17.1-2.67 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyExploration and Mining Geology Search Advanced Search Abstract Gold-bearing mineralization at Anomaly A occurs in polydeformed Ordovician turbidites of the Kendall Mountain Formation of the St. Croix belt in southwestern New Brunswick, and is hosted by WSW-trending, shallow-dipping, brittle–ductile high-strain zones associated with the latest stage of the second of four regional deformation events. Gold-bearing syn-deformational stockwork, massive, and multiply brecciated quartz-sulfide veined zones form irregular pods and sheets up to several meters thick, which contain arsenopyrite, pyrrhotite, pyrite, stibnite, and a variety of rare minerals that are gold-bearing. Mineralized zones are enveloped by locally auriferous, weakly to intensely altered wall rock. Vein paragenesis includes: (1) early (pre- to syn-D2) quartz-chlorite veins that are largely the product of migration of quartz by pressure solution; (2) crosscutting, multiphase, vuggy quartz-sulfide veins that contain most of the gold and are interpreted to be structurally controlled; (3) late, crosscutting, nondeformed, non-gold-bearing veins containing laumontite, chlorite, muscovite, quartz, fluorite, and base metal sulfides. Carbonate-poor alteration associated with zones of gold mineralization is lithology-specific, and appears to reflect overprinting of multiple events. Major elements removed during alteration include Si, Na, Mn, and Mg. The minor and trace elements removed include Co, Li, Sc, and possibly Sr, Ni, and Zn. Minor and trace elements added include Au, Ag, As, Sb, S, and possibly F, Cu, Pb, and Zr. On the basis of proximity, time constraints, and a similar ore mineral assemblage, gold mineralization at Anomaly A is interpreted to be a distal equivalent of the intrusion-related gold mineralization at the nearby Clarence Stream Main zone deposit. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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 score0.060
Threshold uncertainty score0.998

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 science0.0000.000
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 head0.019
GPT teacher head0.189
Teacher spread0.170 · 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