Summary

We demonstrate a minor inconsistency in the appendix of ‘The magnetotelluric phase tensor’ by Caldwell et al. that can lead to incorrect results, and provide a simple solution for this problem.

Since its publication the phase tensor has become an important tool to analyse magnetotelluric data. The reason for this success is, that it is not affected by galvanic distortion and does not make any assumptions about the conductivity structure in the subsurface (Caldwell et al. 2004). However the discussion in the appendix on how to treat the problematic case of a negative determinant is misleading and leads to incorrect expressions when used to calculate the two invariants Φmax and Φmin.

Given the magnetotelluric transfer function Z = X+iY the phase tensor is given by
1
This real second rank tensor can also be expressed in term of three rotational invariants and one rotation angle. In the appendix of Caldwell et al. (2004) the formulae to calculate the invariants Φmax, Φmin and β are given as
2
3
4
5
6
7
an equivalent definition for Φmax and Φmin is given by Bibby (1986, 2005),
8
9
10
11
In certain cases the determinant of the phase-tensor graphic can become negative. The recommendation by Caldwell et al. is to use the absolute value graphic in these cases instead to avoid problems while calculating the intermediate quantity Φ2 which should be real. Through this manipulation the expressions for Φmax and Φmin become incorrect for graphic. Short algebraic manipulation of eq. (5) shows that in this case
12
13
14
and similarly for Φmin. There are two simple ways to avoid problems with negative determinants: Either use the formulae (10) and (11) given by Bibby (2005) that avoid the calculation of the determinant altogether, or circumvent the calculation of Φ2 by inserting (3) into (5) and (6). The resulting expressions are
15
16
and are correct in all cases.

References

Bibby
H.M.
Caldwell
T.G.
Brown
C.
,
2005
.
Determinable and non-determinable parameters of galvanic distortion in magnetotellurics
,
Geophys. J. Int.
,
163
,
915
930
.

Bibby
H.M.
,
1986
.
Analysis of multiple-source bipole-quadripole resistivity surveys using the apparent resistivity tensor
,
Geophysics
,
51
(
4
),
972
983
.

Caldwell
T.G.
Bibby
H.M.
Brown
C.
,
2004
.
The magnetotelluric phase tensor
,
Geophys. J. Int.
,
158
,
457
469
.