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Record W1613661739 · doi:10.1029/2007gc001726

Microstructures in Hole 1274A peridotites, ODP Leg 209, Mid‐Atlantic Ridge: Tracking the fate of melts percolating in peridotite as the lithosphere is intercepted

2008· article· en· W1613661739 on OpenAlexaboutno aff
Guenter Suhr, P. B. Kelemen, Holger Paulick

Bibliographic record

VenueGeochemistry Geophysics Geosystems · 2008
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersDeutsche Forschungsgemeinschaft
KeywordsPeridotiteGeologyLithosphereOlivineMantle (geology)MassifGeochemistryPartial meltingSpinelBasaltAsthenospherePetrologyTectonicsPaleontology

Abstract

fetched live from OpenAlex

We report the microstructures of harzburgites and dunites from ODP Leg 209, Hole 1274A, 15°39′N on the Mid‐Atlantic Ridge. A set of features in these peridotites is so unaffected by plastic flow that it must have formed very late by magmatic processes. We believe that the microstructures record the interaction between a peridotite and a percolating melt as the thermal boundary layer was progressively intercepted. The following chronology for the microstructures is derived: Group 1, resorption of orthopyroxene (opx) associated with olivine precipitation, enhanced by a migrating melt; Group 2, conversion of opx to clinopyroxene (cpx) by a percolating melt; Group 3, precipitation of cpx and spinel as intricate intergrowth (symplectite), associated with olivine dissolution, from an interstitial melt. For these reactions the ratio of melt generated to melt consumed is progressively decreasing, as expected during progressive freezing of asthenosphere. Pristine reaction microstructures analogous to Site 1274A are also found in the Lanzo Massif (Italy) and the Little Port Complex (Canada). For all three settings we infer (1) slow spreading conditions and (2) an ancient depletion event. We thus infer that preservation of the described microstructures is favored by slow spreading and a previous depletion. Slow spreading may be required since it avoids the tectonic overprint during ductile corner flow generally inferred for fast spreading ridges. Slow spreading does not tend, however, to generate highly depleted residues because a thick lithospheric lid limits the extent of melting. Residues will thus tend to be lherzolitic, not harzburgitic. However, lherzolites have a lower permeability for mafic melts than harzburgites. In order to generate the percolation‐dominated microstructures of Site 1274A, a harzburgitic host rock appears favorable. This may now explain the need for an ancient depletion event since only then can harzburgitic residues occur at the top of the mantle column during slow spreading conditions.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.052
Threshold uncertainty score0.104

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
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 head0.011
GPT teacher head0.198
Teacher spread0.188 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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

Citations51
Published2008
Admission routes1
Has abstractyes

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