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- W4200118845 abstract "Abstract Earthquakes can trigger increased degassing in hydrogeological systems. Many of these systems return to preseismic conditions after months, but sometimes postseismic degassing lasts for years. The factors controlling such long-lasting degassing are poorly known. I explored the potential role of diverse triggering mechanisms (i.e., dynamic and static stress changes, volumetric strain) for three large earthquakes that induced postseismic degassing (the Wenchuan [China], Maule [Chile], and Gorkha [Nepal] earthquakes). The lessons from this study suggest that hydrogeological systems can respond to earthquakes in various ways, and different causal mechanisms can play a role. Persistent increased CO2 flux from hot springs has been documented after the Gorkha earthquake. These hot springs had their feeder systems dominantly unclamped, suggesting that sufficiently large normal stress changes may sustain late postseismic degassing. The results of this study are twofold: (1) they show a spatial correlation between unclamping stress and increased gas flow, and (2) they provide an explanation for protracted increased degassing." @default.
- W4200118845 created "2021-12-31" @default.
- W4200118845 creator A5048370392 @default.
- W4200118845 date "2021-12-15" @default.
- W4200118845 modified "2023-09-23" @default.
- W4200118845 title "Can coseismic static stress changes sustain postseismic degassing?" @default.
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- W4200118845 doi "https://doi.org/10.1130/g49465.1" @default.
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