Evidence map›Paper›PMID 42778631›Full record

ArticleNature communications2026

Crustal weakening before rupture at volcanoes after long repose.

Eric L Newland, Christopher R J Kilburn

Abstract read
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

0numbers the graph read from it
0cells of the map it votes in
0citing 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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

2 authors.

Eric L NewlandUCL Hazard Centre, Department of Earth Sciences, University College London, London, UK. px26843@bristol.ac.uk.ORCID http://orcid.org/0000-0003-3501-8115
Christopher R J KilburnUCL Hazard Centre, Department of Earth Sciences, University College London, London, UK.ORCID http://orcid.org/0000-0003-4961-2123

Funding

RCUK | Natural Environment Research Council (NERC) NE/X000133/1
6 · The paper itself

Abstract

At volcanoes reawakening after prolonged quiescence, local seismicity commonly increases before eruption. The earthquakes occur as crust extends over a zone of pressurising fluid several kilometres underground. The deformation causes existing faults to slip and new fractures to open. An eruption is most likely when the fractures grow large enough to rupture the crust. Fracture growth coincides with a net decrease in the elastic energy stored in the crust. Here we present a method for following changes in stored energy through a balance between the energy supplied by the pressure source and lost by seismicity. We test the method against unrest sequences at two large calderas, Sierra Negra and Campi Flegrei. The results provide a practical procedure for identifying the onset of fracture growth and, hence, for recognising an increased potential for crustal rupture.

Identifiers

PMID42778631
PMCPMC13601623

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.