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Record W1600690834 · doi:10.1111/rge.12063

<scp><scp>U–Pb</scp></scp> Ages for Zircon Grains from <scp>N</scp>sanaragati Alluvial Gem Placers: Its Correlation to the Source Rocks

2015· article· en· W1600690834 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.

Bibliographic record

VenueResource Geology · 2015
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of New Brunswick
Fundersnot available
KeywordsZirconGeologyGeochemistryMaficThoriumAlluviumUraniumTrace elementTributaryMineralogyGeomorphology

Abstract

fetched live from OpenAlex

Abstract The M amfe B asin is located in the SW of C ameroon and is an extension of the much bigger B enue T rough in the SE of N igeria. Along the A senem R iver and its tributaries in the western part of the M amfe B asin (close to the border with N igeria) gem placers yielding big zircon grains were found in recent river sediments close to N sanaragati. In order to determine the source area and to establish a possible correlation between the zircons found in the N sanaragati placers and rocks surrounding the M amfe B asin 56 detrital zircon grains were analysed regarding their U – P b ages and selected trace element contents by LA‐ICP – MS techniques. Possible source areas are rocks from the B enue T rough in the W est and from the C ameroon V olcanic L ine ( CVL ) in the SE of the study area. Based on microscopic analyses it was possible to distinguish two groups of zircons: reddish and non‐reddish ones, where the latter group comprises color variations from brown to orange, yellow to even colorless. In general, the detrital zircons show high hafnium values (4576 to 12565 ppm) and very variable thorium (7.8 to 1565 ppm) and uranium values (13.4 to 687 ppm). The T h/ U ratios vary from 0.4 to 2.3, allowing correlations for some zircon grains to kimberlitic, granitic or syenitic affinities. It was also possible to distinguish zircon grains crystallised in mafic mantle‐derived melts from those crystallised in felsic melts, e.g. from continental rift‐related magmatic systems. In general, the U – Pb zircon ages obtained range from 11.7 to 1949 Ma. All zircons of the reddish group yielded almost similar ages resulting in a C oncordia age of 12.4 Ma (Serravallian), an age unknown from the M amfe B asin so far. The group of non‐reddish zircons showed various ages ranging from Serravallian to Orosirian. It was possible to correlate the youngest ages with rocks known from intrusions along the CVL , dated with K / A r or A r/ A r methods. The most probable sources were M ount B amenda and M ount B ambouto in the east of the M amfe B asin. Cretaceous ages are interpreted as re‐recycled clastic sediments whose original source had been rocks in the south and the north of the B enue T rough and who had been eroded and deposited within the catchment area of the A senem river system in the M amfe B asin in post‐ C retaceous times. The oldest ages are assumed to represent the pan‐ A frican and pre‐pan‐ A frican basement of the M amfe basin.

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)0.001
metaresearch head score (Gemma)0.009
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMetaresearch, Meta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.497
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.009
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0000.002

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 head0.023
GPT teacher head0.215
Teacher spread0.192 · 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