Subduction Zone and Tsunami Processes

I am interested in understanding earthquake and tsunami hazards in major subduction zones around the world, e.g., East Japan, Nankai Trough, Chile, Peru, Cascadia, Alaska, Sumatra, New Zealand, etc. One of the significant questions I hope to address is the tsunamigenic processes of shallow megathrust and outer wedge of the forearc, and the associated tsunami propagation and coastal inundation processes. I am also interested in the rheology and heterogeneity of deeper megathrusts and their implications for seismic behavior and coastal shaking.

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Junle Jiang
Postdoctoral Scholar in Geophysics

My research interests include crustal deformation, earthquake dynamics, and natural hazards.

Publications

The 2016 Pedernales earthquake (MW=7.8) ruptured a portion of the Colombia–Ecuador subduction interface where several large …

The 2006 Mw 7.8 Java earthquake was a tsunami earthquake, exhibiting frequency-dependent seismic radiation along strike. High-frequency …

Megathrust earthquakes tend to be confined to fault areas locked in the interseismic period and often rupture them only partially. For …

Diverse observations from the 2011 Mw 9.0 Tohoku-oki earthquake pointed to large coseismic fault slip proximal to the Japan Trench. …

The 2004 Mw 9.1?9.3 Sumatra-Andaman earthquake is one of the largest earthquakes of the modern instrumental era. Despite considerable …

Modeling strong ground motions from great subduction zone earthquakes is one of the great challenges of computational seismology. To …