The organization of seismicity on fault networks.
Although models of homogeneous faults develop seismicity that has a Gutenberg-Richter distribution, this is only a transient state that is followed by events that are strongly influenced by the nature of the boundaries. Models with geometrical inhomogeneities of fracture thresholds can limit the siz...
I tiakina i:
| I whakaputaina i: | Proc Natl Acad Sci U S A |
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| Kaituhi matua: | |
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
National Academy of Sciences
1996
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| Ngā marau: | |
| Urunga tuihono: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC39444/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607672/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.93.9.3830 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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