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Record W2115088847 · doi:10.3906/yer-0806-6

Mineral Chemistry and Petrochemistry of Post-Collisional Tertiary Mafic to Felsic Cogenetic Volcanics in the Ulubey (Ordu) Area, Eastern Pontides, NE Turkey

2009· article· en· W2115088847 on OpenAlexafffund
İ̇rfan Temizel, Mehmet Arslan

Bibliographic record

VenueTURKISH JOURNAL OF EARTH SCIENCES · 2009
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsDomtar (Canada)
FundersKeele UniversityKocaeli ÜniversitesiKaradeniz Teknik ÜniversitesiSivas Cumhuriyet ÜniversitesiOrta Doğu Teknik ÜniversitesiMcGill University
KeywordsLileGeologyGeochemistryPlagioclasePhenocrystHornblendeVolcanic rockBiotiteMaficFractional crystallization (geology)AndesiteBasaltVolcano

Abstract

fetched live from OpenAlex

Post-collisional Tertiary volcanic rocks in the Ulubey (Ordu) area at the western edge of the eastern Pontides palaeo-arc are divided into four suites. The Yenisayaca basalt (TB) contains plagioclase (An_{61-83}), clinopyroxene (Wo_{42-44}En_{39-41}Fs_{15-18}) and olivine phenocrysts and titanomagnetite microphenocrysts, whereas the Çatal Tepe and Elekçioğlu Tepe suite (ÇES), Işık Tepe suite (ITS) and andesite/ trachyandesite suite (ATS) rocks include plagioclase (An_{23-78}), clinopyroxene (Wo_{27-48}En_{37-55}Fs_{11-26}), hornblende (Mg#= 0.63-0.76), biotite (Mg#= 0.63-0.82), sanidine phenocrysts and titanomagnetite and apatite microphenocrysts. Petrochemically, the volcanic rocks show tholeiitic-alkaline to the calc-alkaline affinities, and have medium to high-K contents. Most samples have low Mg#, Cr, and Ni, which indicates that they have undergone significant fractional crystallization from mantle-derived melts. The geochemical variations can be explained by fractionation of common mineral phases such as clinopyroxene ± plagioclase ± magnetite in the Yenisayaca basalt, and hornblende + biotite + plagioclase ± magnetite ± apatite ± sanidine in the Çatal Tepe and Elekçioğlu Tepe suite, Işık Tepe suite and andesite/trachyandesite suite rocks. N-Type MORB-normalized trace element patterns show that Ulubey volcanic rocks are enriched in LILE and to a lesser extent in Th and Ce, but depleted in Zr, Y and TiO_2. Besides, the rocks have depletion in Nb and Ta relative to LILE, moderate LREE/HREE ratios and high Th/Yb ratios, all of which indicate that parental magma(s) probably derived from an enriched source region (probably lithospheric mantle) which was previously modified by fluids. The C1-chondrite-normalized REE patterns are concave with low to medium enrichment, indicating similar source areas for the Yenisayaca Basalt, Çatal Tepe and Elekçioğlu Tepe suite, Işık Tepe suite and andesite/trachyandesite suite. The REE patterns also imply that negative Eu anomalies are probably associated with plagioclase fractionation in the evolution of the rocks.

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)0.001
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 score0.070
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.010
GPT teacher head0.205
Teacher spread0.195 · 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

Citations30
Published2009
Admission routes2
Has abstractyes

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