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Record W2888881730 · doi:10.7939/r35s70

Conditions of diamond formation and preservation from on- and off-craton settings

2011· article· en· W2888881730 on OpenAlexaboutno aff
Lucy Hunt

Bibliographic record

VenueUniversity of Alberta Library · 2011
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsCratonDiamondGeologyEarth scienceMetallurgyMaterials sciencePaleontology

Abstract

fetched live from OpenAlex

The Renard kimberlites (52°48’26N, 72°14’52W: Quebec, Canada) are typical for primary diamond deposits: being located within Archean basement (Superior craton). Pb-Pb isotope data of clinopyroxenes also suggests an Archean age (~2.7Ga) for the subcratonic lithospheric mantle (SCLM). The Carolina Kimberlite (11°29’5S, 61°1’30W: Rondônia State, Brazil) is unconventional, being located within Proterozoic basement (Amazon “craton”). Whilst there are no age constraints on the SCLM, a post-Archean setting is consistent with a lack of harzburgitic garnets. Renard xenolith/xenocryst geothermobarometry suggests, at the time of kimberlite emplacement (~632Ma), an ~190km thick lithosphere with a “cold” (38mW/m2) model conductive geotherm was present. Geothermobarometry on Carolina clinopyroxene grains derived from surficial samples and from kimberlite core indicates two geothermal gradients: a hotter 44mW/m2, and a colder 38mW/m2 geotherm. Grains from the kimberlite core exclusively reflect the colder geotherm, whereas clinopyroxene from surficial samples derive from both gradients. It is proposed that the implied change in geotherm reflects a large scale heating episode which may relate to the opening of the South Atlantic. Diamond inclusion and nitrogen thermometry data from both Renard and Carolina indicate normal mantle residence temperatures, predominantly between 1100-1200oC. At Renard, the xenoliths/xenocrysts and diamond inclusions indicate a peridotite dominated SCLM, with only a minor eclogitic population. Mineral inclusions also document an unusually high abundance of coesite. We propose the presence of SiO2 was caused by an extreme influx of CO2 into peridotitic SCLM, causing progressive carbonation reactions, locally consuming all olivine, orthopyroxene, and clinopyroxene and leaving free SiO2. Diamonds from Carolina have high nitrogen contents and, in part, highly negative carbon isotopic values suggesting an eclogitic paragenesis. This is also indicated by eclogitic garnet xenocrysts (13% of the garnet population), of which just over half have high sodium (>0.07wt% Na2O), considered to be an indication of increased depth and higher diamond potential. Xenoliths/xenocrysts sampled by the Renard kimberlites indicate an evolving melt pervasively re-fertilized an originally strongly depleted lithospheric mantle with respect to highly and moderately incompatible trace elements. Less pervasive fluid style metasomatism, as indicated by selective re-enrichment of highly incompatible elements, occurred within a depth range of 125-170km.

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 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 score0.014
Threshold uncertainty score1.000

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 communication0.0000.001
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.016
GPT teacher head0.145
Teacher spread0.129 · 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.

Study designObservational
Domainnot available
GenreEmpirical

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

Citations1
Published2011
Admission routes1
Has abstractyes

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