Abstract

An accurate viscosity structure is critical to truthfully modeling lithosphere dynamics. Here, we report an attempt to infer the effective lithospheric viscosity from a high-resolution magnetotelluric (MT) survey across the western United States. The high sensitivity of MT fields to the presence of electrically conductive fluids makes it a promising proxy for determining mechanical strength variations throughout the lithosphere. We demonstrate how a viscosity structure, approximated from electrical resistivity, results in a geodynamic model that successfully predicts short-wavelength surface topography, lithospheric deformation, and mantle upwelling beneath recent volcanism. We further show that this viscosity is physically consistent with and better constrained than that derived from laboratory-based rheology. We conclude that MT imaging provides a practical observational constraint for quantifying the dynamic evolution of the continental lithosphere.

Highlights

  • An accurate viscosity structure is critical to truthfully modeling lithosphere dynamics

  • Previous conceptual models of rifting that highlight variations in strain appear to mimic patterns seen in the midcrustal electrical conductivity under similar circumstances [25]. We propose that these high-conductivity patterns (Fig. 1, A and B) represent low-viscosity regions owing to consequences of past deformation of the continental lithosphere

  • We looked for an effective lithospheric viscosity structure resembling the spatial pattern of the MT image that satisfies the available constraints

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Summary

EÃ þ PV RT

Ð1Þ where d is grain size; COH, water fugacity; E* and V *, activation energy and activation volume, respectively; P and T, pressure and temperature, respectively; R, the ideal gas constant; and A, m, n, and r, all laboratory-derived parameters [23]

The electrical resistivity model takes a similar form r
AND NOTES
Findings
Spiral density waves in a young protoplanetary disk
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