Page 2: Research news on aftershock

An aftershock is a seismic event that follows a larger mainshock in the same general region and results from the continued adjustment of the crust to the stress changes induced by the main rupture. Aftershocks typically occur on or near the mainshock fault or on nearby faults perturbed by the stress redistribution. They exhibit characteristic temporal decay in frequency and magnitude, commonly described by Omori-type laws, and spatial clustering around the mainshock rupture zone. Aftershock sequences provide critical information on fault properties, stress transfer, and ongoing deformation, and are central to short-term seismic hazard assessment following major earthquakes.

Powerful 6.2-magnitude quake hits off Istanbul coast

Hours after a 6.2 magnitude earthquake shook Turkey's biggest city, sending panicked residents racing onto the streets, Istanbul remained on edge late Wednesday as a string of aftershocks continued to rattle nerves.

Seismologists share early analyses of Myanmar earthquake

The 28 March magnitude 7.7 Mandalay, Burma (Myanmar) earthquake caused widespread and severe damage in Myanmar and neighboring countries such as Thailand, with more than 5,000 casualties now confirmed. At the Seismological ...

Turkey-Syria temblors reveal missing piece in earthquake physics

The 2023 Kahramanmaraş earthquake struck southern Turkey and Syria along the East Anatolian Fault. The magnitude 7.8 quake and its magnitude 7.5 aftershock devastated the region, killing tens of thousands of people and destroying ...

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