The influence of small stresses on the dynamics of glaciers and subduction zones
The fast flow of glaciers and rupture of earthquakes on subduction zones both occur at interfaces notoriously difficult to observe. When slip events occur on such interfaces, elastic energy is radiated in the form of seismic waves. Here, we analyze these and other signals, such as continuous GPS, fo...
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Format: | Other/Unknown Material |
Language: | English |
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eScholarship, University of California
2012
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Online Access: | https://escholarship.org/uc/item/5jb9839b |