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Microphysical Modeling of Carbonate Fault Friction at Slip Rates Spanning the Full Seismic Cycle

Laboratory studies suggest that seismogenic rupture on faults in carbonate terrains can be explained by a transition from high friction, at low sliding velocities (V), to low friction due to rapid dynamic weakening as seismic slip velocities are approached. However, consensus on the controlling phys...

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Detaylı Bibliyografya
Yayımlandı:J Geophys Res Solid Earth
Asıl Yazarlar: Chen, Jianye, Niemeijer, A. R., Spiers, Christopher J.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: John Wiley and Sons Inc. 2021
Konular:
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC8047899/
https://ncbi.nlm.nih.gov/pubmed/33868888
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2020JB021024
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