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Record W2807196716 · doi:10.1144/sp472.11

Geochemical and temporal provinciality of the magmatism of the eastern Parnaíba Basin, NE Brazil

2018· article· en· W2807196716 on OpenAlexfundno aff
Mônica Heilbron, Eliane Guedes, Miguel Ângelo Mané, Cláudio de Morisson Valeriano, Miguel Tupinambá, Júlio César Horta de Almeida, Luiz Guilherme do Eirado Silva, Beatriz Paschoal Duarte, Jorge Carlos Dela Favera, Adriano R. Viana

Bibliographic record

VenueGeological Society London Special Publications · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersFundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de JaneiroUniversidade do Estado do Rio de JaneiroPetrobrasConselho Nacional de Desenvolvimento Científico e TecnológicoUniversity of Toronto
KeywordsMagmatismGeologyStructural basinGeochemistryPaleontologyTectonics

Abstract

fetched live from OpenAlex

Abstract This paper presents new field, petrographic, geophysical, geochemical and geochronological data for the felsic and mafic magmatism of the eastern Parnaíba Basin, integrating previously published data with new surface data acquired within the scope of the Cooperation Program developed by UERJ-Petrobras. New precise 40 Ar– 39 Ar Cambrian ages ( c. 508–506 Ma) were obtained for the felsic volcanic to subvolcanic rocks associated with intracontinental rift sediments in the São Raimundo Nonato area in the SE of the basin. The new results include the detection of three different basic magmatic pulses at c. 181, 126 and 118 Ma, related, respectively, to Central Atlantic Magmatic Province magmatism, the Sardinha large igneous province and the break-up period for the equatorial basins. The eastern side of the basin contrasts with the western side and shows a predominance of outcropping sills of Sardinha age. Most of these rocks are quartz tholeiites, but two samples ( c. 118 Ma) are olivine tholeiites. This paper provides the first description of a clear chemical provinciality of the Sardinha tholeiitic magmatism in the eastern Parnaíba Basin, similar to that described in the Paraná Basin. Low-TiO 2 suites, independent of age, occur on the northwestern side of the Senador Pompéu–Coccoci lineament, whereas high-TiO 2 suites, including the Ceará Mirim dyke swarm in the basement to the east, are located SE of this lineament. The duality of geochemical signatures reproduces the basement signatures of the opposite sides of the Senador Pompéu suture zone, suggesting, at least in part, that the composition of the sub-lithospheric continental mantle of these two domains played a part in the development of Cretaceous magmatism in the Parnaíba Basin. Supplementary material: Geophysical and geochemical data provided by Petrobras and subsequent analysis. Supplementary material available online at https://doi.org/10.6084/m9.figshare.c.4117985

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)0.001
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 score0.104
Threshold uncertainty score0.206

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.014
GPT teacher head0.215
Teacher spread0.202 · 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

Citations26
Published2018
Admission routes1
Has abstractyes

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