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What is Fluid-Induced Earthquake Swarms in MER about?

This research article investigates the role of fluid migration in inducing earthquake swarms in the Main Ethiopian Rift (MER) using high-resolution earthquake relocation and cross-correlation analysis. The findings indicate that seismicity within the rift is primarily fluid-induced, characterized by short swarms of similar earthquakes, while seismicity on the rift margin is driven by tectonic stress. The study highlights the significance of deep-sourced fluids, such as mantle-derived CO2, in influencing sei

Author

Aklilu

Language

EN