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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...
Tallennettuna:
| Julkaisussa: | Geophys Res Lett |
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| Päätekijät: | , , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
John Wiley and Sons Inc.
2021
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8243972/ https://ncbi.nlm.nih.gov/pubmed/34219831 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2021GL092417 |
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