Does rapid change in ice loading modulate strain accumulation and release in glaciated, tectonically active regions

There are major glaciated regions of the world that are also seismologically active. Changes in the thickness of ice due to glacier surges, advances, or retreats produce stress changes that may be a significant fraction of the tectonic stress accumulated during an earthquake cycle. The changes in ic...

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Veröffentlicht in:	Geophysical research letters 1993-10, Vol.20 (19), p.2123-2126
1. Verfasser:	Cohen, Steven C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Faults Glaciers Seismic phenomena Shear stress Strain Strain rate Stresses Tectonics
Online-Zugang:	Volltext
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