Evidence map›Paper›PMID 37438364›Full record

ArticleNature communications2023

Volcanic evolution of an ultraslow-spreading ridge.

H H Stubseid, A Bjerga, H Haflidason, L E R Pedersen, R B Pedersen

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

5 authors.

H H Stubseid *Center for Deep Sea Research and Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway. havard.stubseid@uib.no.ORCID http://orcid.org/0000-0002-6363-1198
A Bjerga *Center for Deep Sea Research and Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway.ORCID http://orcid.org/0000-0001-5541-3898
H HaflidasonCenter for Deep Sea Research and Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway.ORCID http://orcid.org/0000-0002-7782-8856
L E R PedersenCenter for Deep Sea Research and Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway.
R B PedersenCenter for Deep Sea Research and Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Nearly 30% of ocean crust forms at mid-ocean ridges where the spreading rate is less than 20 mm per year. According to the seafloor spreading paradigm, oceanic crust forms along a narrow axial zone and is transported away from the rift valley. However, because quantitative age data of volcanic eruptions are lacking, constructing geological models for the evolution of ultraslow-spreading crust remains a challenge. In this contribution, we use sediment thicknesses acquired from ~4000 km of sub-bottom profiler data combined with

Identifiers

PMID37438364
PMCPMC10338544

What OpenQuestion holds

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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.