Fluid and melt pathways in the central Chilean subduction zone near the 2010 Maule earthquake (35° ‐ 36° S) as inferred from magnetotelluric data

The subduction zone of central Chile (36° S) has produced some of the world's largest earthquakes and significant volcanic eruptions. Understanding the fluid fluxes and structure of the subducting slab and over‐riding plate can provide insight into the tectonic processes responsible for both seismicity and magmatism. Broadband and long‐period magnetotelluric data were collected along a 350 km profile in central Chile and Argentina and show a regional geoelectric strike of 15±19° east of north. The preferred two‐dimensional inversion model included the geometry of the subducting Nazca plate as a constraint. On the upper surface of the Nazca plate, conductors were interpreted as fluids expelled from the down‐going slab via compaction at shallow depth (C1) and metamorphic reactions at depths of 40‐90 km (C2 and C3). At greater depths (130 km), a conductor (C7) is interpreted as a region of partial melt related to de‐serpentinization in the back‐arc. A resistor on the slab interface (R1) is coincident with a high‐velocity anomaly which was interpreted as a strong asperity which may affect the co‐seismic slip behavior of large megathrust earthquakes at this latitude. Correlations with seismicity suggest slab fluids alter the forearc mantle and define the down‐dip limit of the seismogenic zone. Beneath the volcanic arc, several upper crustal conductors (C4 and C5) represent partial melt beneath the Tatara‐San Pedro Volcano and the Laguna del Maule Volcanic Field. A deeper lower‐crustal conductor (C6) underlies both volcanoes and suggests a connected network of melt in a thermally‐mature lower crust