טוען...
Repeating caldera collapse events constrain fault friction at the kilometer scale
Fault friction is central to understanding earthquakes, yet laboratory rock mechanics experiments are restricted to, at most, meter scale. Questions thus remain as to the applicability of measured frictional properties to faulting in situ. In particular, the slip-weakening distance [Formula: see tex...
שמור ב:
| הוצא לאור ב: | Proc Natl Acad Sci U S A |
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| Main Authors: | , |
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
National Academy of Sciences
2021
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| נושאים: | |
| גישה מקוונת: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8325243/ https://ncbi.nlm.nih.gov/pubmed/34301896 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2101469118 |
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