Evidence map›Paper›PMID 38830886›Full record

ReviewNature communications2024

Earthquake energy dissipation in a fracture mechanics framework.

David S Kammer, Gregory C McLaskey, Rachel E Abercrombie, Jean-Paul Ampuero, Camilla Cattania, Massimo Cocco, Luca Dal Zilio, Georg Dresen, Alice-Agnes Gabriel, Chun-Yu Ke and 3 more

Erratum issuedAbstract readReview
In one paragraph

Review in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 8 papers.

0numbers the graph read from it
0cells of the map it votes in
8citing 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

8 citing papers in PubMed.

  1. Article
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  7. Evolution of the real area of contact during laboratory earthquakes.Proceedings of the National Academy of Sciences of the United States of America · 2025
    Article
  8. Article
4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

13 authors.

David S KammerInstitute for Building Materials, ETH Zurich, Zurich, Switzerland. dkammer@ethz.ch.ORCID http://orcid.org/0000-0003-3782-9368
Gregory C McLaskeySchool of Civil and Environmental Engineering, Cornell University, Ithaca, NY, USA.
Rachel E AbercrombieBoston University, Boston, MA, USA.ORCID http://orcid.org/0000-0003-4515-5420
Jean-Paul AmpueroUniversité Côte d'Azur, Observatoire de la Côte d'Azur, IRD, CNRS, Géoazur, Valbonne, France.ORCID http://orcid.org/0000-0002-4827-7987
Camilla CattaniaDepartment of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA.
Massimo CoccoIstituto Nazionale di Geofisica e Vulcanologia, Rome, Italy.
Luca Dal ZilioEarth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore.ORCID http://orcid.org/0000-0002-5642-0894
Georg DresenHelmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany.ORCID http://orcid.org/0000-0002-3737-2858
Alice-Agnes GabrielScripps Institution of Oceanography, UCSD, La Jolla, USA.ORCID http://orcid.org/0000-0003-0112-8412
Chun-Yu KeDepartment of Geosciences, The Pennsylvania State University, University Park, PA, 16802, USA.ORCID http://orcid.org/0000-0002-4337-3152
Chris MaroneDepartment of Geosciences, The Pennsylvania State University, University Park, PA, 16802, USA.ORCID http://orcid.org/0000-0002-4515-4500
Paul Antony SelvaduraiSwiss Seismological Service, ETH Zurich, Zurich, Switzerland.ORCID http://orcid.org/0000-0002-3846-8333
Elisa TintiIstituto Nazionale di Geofisica e Vulcanologia, Rome, Italy.ORCID http://orcid.org/0000-0002-6942-3592

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Earthquakes are rupture-like processes that propagate along tectonic faults and cause seismic waves. The propagation speed and final area of the rupture, which determine an earthquake's potential impact, are directly related to the nature and quantity of the energy dissipation involved in the rupture process. Here, we present the challenges associated with defining and measuring the energy dissipation in laboratory and natural earthquakes across many scales. We discuss the importance and implications of distinguishing between energy dissipation that occurs close to and far behind the rupture tip, and we identify open scientific questions related to a consistent modeling framework for earthquake physics that extends beyond classical Linear Elastic Fracture Mechanics.

Identifiers

PMID38830886
PMCPMC11148115

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.