Spatiotemporal Evolution of 2024 Klingenthal-Kraslice Swarm Beneath the Eger Rift

Published in Earth & Environment

Go to the profile of Pınar Büyükakpınar
Pınar Büyükakpınar
Seismologist, GFZ Helmholtz Centre for Geosciences
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Spatiotemporal evolution of seismicity beneath the Eger Rift showing two phases of swarm activity: an initial hydro-fracturing phase driven by CO₂-rich fluids, followed by hydro-shearing associated with denser magmatic or brine-rich fluids.

Go to the profile of Pınar Büyükakpınar
Pınar Büyükakpınar
Seismologist, GFZ Helmholtz Centre for Geosciences

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