Effects of galvanic distortion on magnetotelluric data over a three-dimensional regional structure

被引:29
作者
Ledo, J [1 ]
Queralt, P [1 ]
Pous, J [1 ]
机构
[1] Univ Barcelona, Dept Geol Dinam Geofis & Paleontol, E-08028 Barcelona, Spain
关键词
electrical resistivity; magnetotellurics; structural dimensionality; tensor decomposition;
D O I
10.1046/j.1365-246x.1998.00417.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Although the galvanic distortion due to local, near-surface inhomogeneities is frequency-independent, its effect on the magnetotelluric data becomes, in a 3-D structure, frequency-dependent. Therefore, both the apparent resistivity and the phase responses are disturbed, and a correction should be carried out prior to the 3-D interpretation in order to retrieve the 3-D regional impedance tenser. In many cases, the structure is 2-D for depths corresponding to a first range of periods and 3-D for longer periods (called 2-D/3-D). For these cases, a simple method which allows us to retrieve the 3-D regional impedance tensor (except the static shift) is presented. The method proposed uses the Groom & Bailey decomposition of the distortion matrix for the short periods. Three examples are presented: two using synthetic data and one employing real data. These examples show the effect of the galvanic distortion over a regional 2-D/3-D model and the retrieval of the regional transfer functions from the distorted ones.
引用
收藏
页码:295 / 301
页数:7
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