Tension cracks were generated by past megathrust earthquakes along the coastal forearc of Chile-Peru. To explain why elastic rebound in an offshore earthquake...
Contemporary deformation of the Cascadia forearc consists of an elastic interseismic strain build-up as part of the subduction earthquake deformation "cycle"...
For the Nankai Trough and Japan Trench subduction zones, we examine the combined thermal effects of lateral heat exchange by fluid circulation in an oceanic...
In southern Kurile, interseismic contraction observed with Global Navigation Satellite Systems is faster in the volcanic arc than in the forearc. Here, we use...
A smooth subducting seafloor usually leads to a smooth megathrust, which promotes great earthquakes. We present a case study at the northern Manila Trench to...
Mass-balancing voltages from four buried broadband seismometers connected to the NEPTUNE Canada seafloor cable are being recorded at 24-bit resolution. Sites...
The 2012 Mw 7.8 Haida Gwaii earthquake confirmed very oblique subduction and slip partitioning at the southern Queen Charlotte margin. In this study, we...
Bi(Zn 0.5,Ti 0.5)O 3 (BZT) doped Pb(Zr 0.4,Ti 0.6)O 3 (PZT) films were fabricated using a chemical solution deposition method and were characterized...
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