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Abstract: Can magnetotelluric observations along subduction zone margins detect alterations of the fluid interconnection network in the mantle wedge near the slab interface due to pre-, syn- and post seismic event changes in the stress field? (AGU25)

Can magnetotelluric observations along subduction zone margins detect alterations of the fluid interconnection network in the mantle wedge near the slab interface due to pre-, syn- and post seismic event changes in the stress field?

Adam Schultz, Oregon State University, College of Earth, Ocean and Atmospheric Sciences, Corvallis, OR, United States and Xiaolei Tu, Oregon State University, CEOAS, Corvallis, United States; IGG Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
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