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Abstract Earthquakes can alter fluid flow far from a rupture, but the processes that sustain such changes for months remain uncertain. Here we report a sustained increase in gas-phase helium concentration at a thermal spring on the Red River Fault, about 600 kilometres from the 2025 magnitude 7.7 Myanmar earthquake. Minute-scale monitoring recorded intermittent fluctuations before the earthquake and a progressive concentration increase afterwards.
As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.
