Earthquake nucleation and fault slip complexity in the lower crust of central Alaska
Earthquakes start under conditions that are largely unknown. In laboratory analogue experiments and continuum models, earthquakes transition from slow-slipping, growing nucleation to fast-slipping rupture. In nature, earthquakes generally start abruptly, with no evidence for a nucleation process. He...
Główni autorzy: | Tape, C, Holtkamp, S, Silwal, V, Hawthorne, J, Kaneko, Y, Ampuero, JP, Ji, C, Ruppert, N, Smith, K, West, ME |
---|---|
Format: | Journal article |
Wydane: |
Springer Nature
2018
|
Podobne zapisy
-
The Effects of Fault Roughness on the Earthquake Nucleation Process
od: Tal, Yuval, i wsp.
Wydane: (2022) -
The 2002 Denali fault earthquake, Alaska : a large magnitude, slip-partitioned event
od: Eberhart-Phillips, Donna, i wsp.
Wydane: (2013) -
Double-difference adjoint tomography of the crust and uppermost mantle beneath Alaska
od: Chen, Guoxu, i wsp.
Wydane: (2023) -
Xenoliths and the nature of the upper mantle and lower crust Nunivak Island, Alaska.
od: Francis, Donald Michael
Wydane: (2005) -
Kinematic behavior of southern Alaska constrained by westward decreasing postglacial slip rates on the Denali Fault, Alaska
od: Mériaux, Anne-Sophie, i wsp.
Wydane: (2012)