Laboratory observations of slow earthquakes and the spectrum of tectonic fault slip modes
Slow earthquakes, where fault slip is slow, can be large and may help trigger regular earthquakes, but the mechanics of slow slip are not fully understood. Leeman et al.show through laboratory experiments that slow slip behaviour on faults is controlled by the frictional dynamics of the surrounding...
Saved in:
Main Authors: | J. R. Leeman, D. M. Saffer, M. M. Scuderi, C. Marone |
---|---|
Format: | article |
Language: | EN |
Published: |
Nature Portfolio
2016
|
Subjects: | |
Online Access: | https://doaj.org/article/ae43ca8fe16d49b9a92d1e4bd3b20e64 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Earthquake slip surfaces identified by biomarker thermal maturity within the 2011 Tohoku-Oki earthquake fault zone
by: Hannah S. Rabinowitz, et al.
Published: (2020) -
Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust
by: Dibyashakti Panda, et al.
Published: (2018) -
Fault valving and pore pressure evolution in simulations of earthquake sequences and aseismic slip
by: Weiqiang Zhu, et al.
Published: (2020) -
Large fault slip peaking at trench in the 2011 Tohoku-oki earthquake
by: Tianhaozhe Sun, et al.
Published: (2017) -
The role of space-based observation in understanding and responding to active tectonics and earthquakes
by: J.R. Elliott, et al.
Published: (2016)