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This study presents a 3-D magnetotelluric imaging of the electrical resistivity structure beneath the Abaga-Dalinor volcanic field in eastern China, revealing significant geological features such as a high-resistivity layer representing the Precambrian basement and high conductivity anomalies indicating saline fluid zones. The findings suggest that the intraplate volcanism in this region is influenced by pre-existing tectonic weak zones and localized asthenospheric upwelling, potentially linked to the westw

Author

gwdjsk

Language

EN