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Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-20 (2021)
Abstract A model for coseismic groundwater level increase is presented for understanding hydrological responses of wells to seismic waves. Three types of coseismic groundwater level changes were observed in six wells 300–500 m in depth, operated by
Externí odkaz:
https://doaj.org/article/90239c6b98e9469bb6d62ad2c246152d
Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-20 (2021)
A model for coseismic groundwater level increase is presented for understanding hydrological responses of wells to seismic waves. Three types of coseismic groundwater level changes were observed in six wells 300–500 m in depth, operated by the Hot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::50c0656a06102514bc6e47d922641bfc
https://doaj.org/article/90239c6b98e9469bb6d62ad2c246152d
https://doaj.org/article/90239c6b98e9469bb6d62ad2c246152d
Akademický článek
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