Not exact matches
A temperature anomaly of 0.31 °C indicates coseismic
friction was extremely low
during the
earthquake.
Their results, published December 5 in Science, show that
friction on the fault was remarkably low
during the magnitude 9.0 Tohoku - Oki
earthquake that struck off the coast of Japan in March 2011 and triggered a devastating tsunami.
«How
friction evolves
during an
earthquake: By simulating quakes in a lab, engineers study the way that
friction changes along a fault
during a seismic event.»
Highly destructive
earthquakes caused by subduction occur because of excessive
friction that develops
during the sliding process, resulting in a build - up of stress.
Friction dissipates heat during an earthquake; therefore, the fault temperature after an earthquake provides insight into the level of f
Friction dissipates heat
during an
earthquake; therefore, the fault temperature after an
earthquake provides insight into the level of
frictionfriction.
The
friction as two massive plates of the Earth's crust slide past one another is dissipated as heat, so temperature measurements can give scientists a handle on the fault's resistance to sliding
during the
earthquake.