ArticleScientific reports2026
Long period quakes linked to Mefite D'Ansanto (Italy) mantellic CO
Article in Scientific reports, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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.
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.
Who cites it
0 citing papers in PubMed.
No citing paper in PubMed yet.
Corrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
Authors and funding
4 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Mefite D’Ansanto is a remarkable mantle origin CO2 emissions system, and the understanding of the relative source mechanisms is one of the fundamental aspects for the comprehension of the evolution of the southern Apennines active dynamics. Moreover, due to its lively activity in a nearly quiet place, Mefite also represents a natural laboratory for the investigation of hydrothermal system dynamics. The seismic wavefield sourced by these CO2 emissions is complex, characterized by a background stationary hydrothermal tremor, with intermittent superposition wavetrains of variable duration. Here we focus on the transient signals generated by the emissions, which show a spectral content in 0.7–7.0 Hz and a peculiar waveform, described here for the first time. Due to their similarities with Long Period earthquakes occurring in volcanic/hydrothermal systems, we classify them as LP quakes and investigate their propagation and source processes. The Mefite LPs appear to be a mixture of P- and surface waves, generated at a depth slightly greater than that of the hydrothermal tremor and likely associated with bubbling mechanisms.
Indexed as
Identifiers
What OpenQuestion holds
Registered trials
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.