Omori‐like decay of postseismic velocities following continental earthquakes
Abstract Various mechanisms have been proposed to explain the transient, enhanced surface deformation rates following earthquakes. Unfortunately, these different mechanisms can produce very similar surface deformation patterns leading to difficulty in distinguishing between them. Here we return to t...
I tiakina i:
| Ngā kaituhi matua: | , |
|---|---|
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Wiley
2017-04-01
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| Rangatū: | Geophysical Research Letters |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.1002/2017GL072865 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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