Seismic Slip‐Pulse Experiments Simulate Induced Earthquake Rupture in the Groningen Gas Field

Rock materials show dramatic dynamic weakening in large‐displacement (m), high‐velocity (∼1 m/s) friction experiments, providing a mechanism for the generation of large, natural earthquakes. However, whether such weakening occurs during induced M3‐4 earthquakes (dm displacements) is unknown. We perf...

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Detalles Bibliográficos
Autores principales: Hunfeld, Luuk B., Chen, Jianye, Niemeijer, André R., Ma, Shengli, Spiers, Christopher J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Letter
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8243972/
https://www.ncbi.nlm.nih.gov/pubmed/34219831
http://dx.doi.org/10.1029/2021GL092417

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8243972/
https://www.ncbi.nlm.nih.gov/pubmed/34219831
http://dx.doi.org/10.1029/2021GL092417

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