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We invert these data using the presented time-lapse algorithm.
We invert these data to recover the conductivity at depths between 10 km and 1000 km.
We invert this scale such that higher values correspond to better health.
For e - j 2 π n N we invert the imaginary part's sign.
Finally, we invert for the magnetic moments of the sources using the measured magnetic gradient tensor data and forward model.
First, we invert two fault patches (one for the Tokai slow slip and one for the Tohoku afterslip).
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We inverted the pyramid of the organization and made reverse accountability a reality.
"Hey, that looks cool," Max said as we inverted the pan onto a plate and lifted it off.
Then, we inverted the deformations to estimate the open parameter of the sill.
In the first step, we inverted only T zx and T zy without impedance data.
We inverted the observed deformations for the source parameters of the two earthquakes using elastic dislocation modeling.
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