Evidence map›Paper›PMID 41826363›Full record

ArticleScientific data2026

Rheological evolution of a trachybasalt from Mt. Etna under slow cooling.

Fabrizio Di Fiore, Alessandro Vona

Abstract read
In one paragraph

Article in Scientific data, 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.

Fabrizio Di FioreIstituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma 1, Via di Vigna Murata 605, 00143, Roma, Italy. fabrizio.difiore@ingv.it.
Alessandro VonaDipartimento di Scienze, Università degli Studi Roma Tre, L.go San Leonardo Murialdo 1, 00146, Roma, Italy.

Funding

Ministero dell'Università e della Ricerca D53C22001400005Ministero dell'Università e della Ricerca P20222BP7J
6 · The paper itself

Abstract

Understanding the rheological evolution of solidifying magma during its migration through the crust and the subsequent emplacement as lava is critical for assessing volcanic hazards. Crystallization plays a primary role in governing the rheology of low-viscosity basaltic magmas, thereby controlling lava inundation potential. While several studies have addressed this behavior under faster cooling conditions, experimental data bridging the gap toward the quasi-equilibrium regime remain scarce due to the technical challenges of long-duration high-temperature rheometry experiments. This highlights the critical need for new datasets designed to quantify the rheological evolution pertinent to lava flow emplacement conditions. Here, we present a rheological dataset carried out on an Etnean trachybasalt, focusing on low cooling rates (0.1 and 0.5 °C/min) under variable shear strain rates (1-10 s

Identifiers

PMID41826363
PMCPMC13149540

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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.