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- W2093301497 abstract "[1] The electrical structure of the upper mantle beneath the East Pacific Rise (EPR) at 15°45'S is imaged by inverting seafloor magnetotelluric data obtained during the Mantle ELectromagnetic and Tomography (MELT) experiment. The electrical conductivity model shows no evidence for a conductive region immediately beneath the ridge, in contrast to the model previously obtained beneath the EPR at 17°S. This observation can be explained by differences in current melt production along the ridge, consistent with other observations. The mantle to the east of the ridge at 60 -100 km depth is anisotropic, with higher conductivity in the spreading direction compared to the along-strike direction, similar to the 17°S region. The high conductivity in the spreading direction can be explained by a hydrated mantle with strain-induced lattice preferred orientation of olivine or by partial melt preferentially connected in the spreading direction." @default.
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- W2093301497 date "2006-11-16" @default.
- W2093301497 modified "2023-10-17" @default.
- W2093301497 title "Electrical structure beneath the northern MELT line on the East Pacific Rise at 15°45′S" @default.
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- W2093301497 doi "https://doi.org/10.1029/2006gl027528" @default.
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