Rl. Parker et Jr. Booker, OPTIMAL ONE-DIMENSIONAL INVERSION AND BOUNDING OF MAGNETOTELLURIC APPARENT RESISTIVITY AND PHASE MEASUREMENTS, Physics of the earth and planetary interiors, 98(3-4), 1996, pp. 269-282
The properties of the log of the admittance in the complex frequency p
lane lead to an integral representation for one-dimensional magnetotel
luric (MT) apparent resistivity and impedance phase similar to that fo
und previously for complex admittance. The inverse problem of finding
a one-dimensional model for MT data can then be solved using the same
techniques as for complex admittance, with similar results. For instan
ce, the one-dimensional conductivity model that minimizes the chi(2) m
isfit statistic for noisy apparent resistivity and phase is a series o
f delta functions. One of the most important applications of the delta
function solution to the inverse problem for complex admittance has b
een answering the question of whether or not a given set of measuremen
ts is consistent with the modeling assumption of one-dimensionality. T
he new solution allows this test to be performed directly on standard
MT data, Recently, it has been shown that induction data must pass the
same one-dimensional consistency test if they correspond to the polar
ization in which the electric field is perpendicular to the strike of
two-dimensional structure, This greatly magnifies the utility of the c
onsistency test. The new solution also allows one to compute the upper
and lower bounds permitted on phase or apparent resistivity at any fr
equency given a collection of MT data, Applications include testing th
e mutual consistency of apparent resistivity and phase data and placin
g bounds on missing phase or resistivity data, Examples presented demo
nstrate detection and correction of equipment and processing problems
and verification of compatibility with two-dimensional B-polarization
for MT data after impedance tensor decomposition and for continuous el
ectromagnetic profiling data.