Evidence map›Paper›PMID 38914555›Full record

ArticleNature communications2024

Evidence for the formation of silicic lava by pyroclast sintering.

Annabelle Foster, Fabian B Wadsworth, Hugh Tuffen, Holly E Unwin, Madeleine C S Humphreys

Abstract read
In one paragraph

Article in Nature communications, 2024. 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.

Annabelle FosterEarth Science, Durham University, Science Labs, Durham, DL1 3LE, UK. annabelle.foster@durham.ac.uk.ORCID http://orcid.org/0000-0002-1578-5328
Fabian B WadsworthEarth Science, Durham University, Science Labs, Durham, DL1 3LE, UK. fabian.wadsworth@gmail.com.ORCID http://orcid.org/0000-0002-5341-208X
Hugh TuffenLancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK.ORCID http://orcid.org/0000-0001-8829-1751
Holly E UnwinLancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK.ORCID http://orcid.org/0000-0001-6396-7014
Madeleine C S HumphreysEarth Science, Durham University, Science Labs, Durham, DL1 3LE, UK.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Silicic lavas can be produced by the sintering of pyroclasts in the volcanic sub-surface, and then advected out of the vent. Here, we provide evidence for this mechanism preserved in the exposed post-glacial remnants of a silicic volcanic conduit at Hrafntinnuhryggur, Krafla volcano, Iceland. We show that the conduit margins are a clast-supported pumice lapilli tuff deposit that grades continuously into dense obsidian and that the obsidian contains cuspate relict clast boundaries and country rock lithic fragments throughout. Transects of H

Identifiers

PMID38914555
PMCPMC11196653

What OpenQuestion holds

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LicenceCC BY
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Registered trials

None linked

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.