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as appropriate to obtain a good S /N ratio for a given source–receiver geometry. Here, Ex and Ey denote the horizontal electric field components, and Hx and Hy denote the horizontal magnetic field components ...
is implemented in terms of conductivity, results are presented in terms of its inverse , resistivity (|$\rho $|), to be consistent with much of the AEM literature. In addition to the layered -earth model ...
, gravimetry and electromagnetic data can identify contemporary melt zones, magma reservoirs and/or crystal mushes. These techniques complement seismic reflection data and rock magnetic analyses that delimit ...
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