5 (568) In stock
Temporary slip speed increases with durations of 1–3 h were identified during short-term slow slip events in records of borehole and laser strainmeters in the Tokai region, Japan. They were found by searching for peaks of correlation coefficients between stacked strain data and ramp functions with rise times of 1 and 2 h. Although many of the strain steps were considered due to noise, some strain steps occurred with simultaneous activation of the deep tectonic tremors and shared source areas with the tremors. From 2016 to 2022, we observed five strain steps with simultaneous activation of tectonic tremors and coincidence of source locations with the tremors. Those strain steps occurred during short-term slow slip events and were temporary slip speed increases of the slow slip events. Those strain steps seemed to be related to successive occurrences with source migration of short-term slow slip events. The detrended strain steps corresponded to plate boundary slip events of moment magnitude around 5, which was consistent with the scaling law of slow earthquakes. Graphical Abstract
PDF) A scaling law for slow earthquakes
Slow-slip, slow earthquakes, period-two cycles, full and partial
Long-term slow slip events with and without tremor activation in
Properly calculating estat phtest in the presence of stratified hazards
Long-term slow slip events with and without tremor activation in
Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip
Short-term interaction between silent and devastating earthquakes
Articles Earth, Planets and Space
What are slow slips? — Science Learning Hub
Long-term slow slip events with and without tremor activation in
Properly calculating estat phtest in the presence of stratified hazards
EARLY EXPERIENCE OF THE FITBONE NAIL IN ADOLESCENCE: A LEARNING CURVE
Integrated rupture mechanics for slow slip events and earthquakes
EARLY EXPERIENCE OF THE FITBONE NAIL IN ADOLESCENCE: A LEARNING CURVE
