..for earthquake dynamic rupture simulations.

Read more at:
agupubs.onlinelibrary.wiley.com/doi/10.1029/...

An online documentation providing step-by-step examples is also available at geoteqpy.readthedocs.io/en/latest/

... simulations into explicit fault surface geometries, using a medial‐axis transform of envelope iso-surfaces.
We show examples across tectonic settings (rifting, strike-slip fault systems, subduction zones), bridging the gap between large-scale geodynamic models and the fault geometries needed..

Thanks @peaseroland.bsky.social! This was just sent out for review so happy for any comments or questions

whereas moderate events reflect transient asperities and short-term variations in fault strength. Our systematic statistics provide new constraints for coupling models and for linking geodesy with seismic hazard assessment. We welcome comments and discussion!

We find that large events (Mw ≥ 7.5) systematically rupture strongly coupled regions, while smaller events rupture more variably, often in weakly coupled areas. This magnitude-dependent pattern may suggest that great earthquakes primarily release long-term accumulated strain,

All of us and our science look better than Captin Underpants.

San Diego Supercomputer Center for the behind-the-scenes tour. Looking forward to next year, when we will organize a large-scale Tandem user training!

⚠️ Tsunamis can be a series of powerful surges capable of creating dangerous currents for hours. Stay alert and keep away from the beach and shoreline until officials give the all-clear.

🌏 USGS Earthquake information: on.doi.gov/4faXyBW
🌊 NOAA Tsunami information: bit.ly/49qPWZ5