The magnetotelluric phase tensor

被引:1006
作者
Caldwell, TG
Bibby, HM
Brown, C
机构
[1] Inst Geol & Nucl Sci, Lower Hutt, New Zealand
[2] Natl Univ Ireland Univ Coll Galway, Appl Geophys Unit, Galway, Ireland
关键词
electromagnetic methods; galvanic distortion; magnetotellurics;
D O I
10.1111/j.1365-246X.2004.02281.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
The phase relationships contained in the magnetotelluric (MT) impedance tensor are shown to be a second-rank tensor. This tensor expresses how the phase relationships change with polarization in the general case where the conductivity structure is 3-D. Where galvanic effects produced by heterogeneities in near-surface conductivity distort the regional MT response the phase tensor preserves the regional phase information. Calculation of the phase tensor requires no assumption about the dimensionality of the underlying conductivity distribution and is applicable where both the heterogeneity and regional structure are 3-D. For 1-D regional conductivity structures, the phase tensor is characterized by a single coordinate invariant phase equal to the 1-D impedance tensor phase. If the regional conductivity structure is 2- D, the phase tensor is symmetric with one of its principal axes aligned parallel to the strike axis of the regional structure. In the 2- D case, the principal values (coordinate invariants) of the phase tensor are the transverse electric and magnetic polarization phases. The orientation of the phase tensor's principal axes can be determined directly from the impedance tensor components in both 2-D and 3-D situations. In the 3-D case, the phase tensor is nonsymmetric and has a third coordinate invariant that is a distortion-free measure of the asymmetry of the regional MT response. The phase tensor can be depicted graphically as an ellipse, the major and minor axes representing the principal axes of the tensor. 3-D model studies show that the orientations of the phase tensor principal axes reflect lateral variations (gradients) in the underlying regional conductivity structure. Maps of the phase tensor ellipses provide a method of visualizing this variation.
引用
收藏
页码:457 / 469
页数:13
相关论文
共 26 条
[1]  
[Anonymous], 1986, NUMERICAL RECIPES C
[2]  
BAHR K, 1988, J GEOPHYS-Z GEOPHYS, V62, P119
[3]   GEOLOGICAL NOISE IN MAGNETOTELLURIC DATA - A CLASSIFICATION OF DISTORTION TYPES [J].
BAHR, K .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1991, 66 (1-2) :24-38
[4]   GEOPHYSICAL EVIDENCE ON THE STRUCTURE OF THE TAUPO VOLCANIC ZONE AND ITS HYDROTHERMAL CIRCULATION [J].
BIBBY, HM ;
CALDWELL, TG ;
DAVEY, FJ ;
WEBB, TH .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1995, 68 (1-3) :29-58
[5]   ANALYSIS OF MULTIPLE-SOURCE BIPOLE-QUADRIPOLE RESISTIVITY SURVEYS USING THE APPARENT RESISTIVITY TENSOR [J].
BIBBY, HM .
GEOPHYSICS, 1986, 51 (04) :972-983
[6]  
BIBBY HM, 1998, J GEOPHYS RES, V81, P69
[7]  
Bruton P, 1994, THESIS NATL U IRELAN
[8]   The instantaneous apparent resistivity tensor: a visualization scheme for LOTEM electric field measurements [J].
Caldwell, TG ;
Bibby, HM .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1998, 135 (03) :817-834
[9]  
Caldwell TG, 2002, GEOPHYS J INT, V151, P755, DOI 10.1046/j.1365-246X.2002.01798.x
[10]   A SIMPLE TECHNIQUE FOR ANALYZING AND PARTLY REMOVING GALVANIC DISTORTION FROM THE MAGNETOTELLURIC IMPEDANCE TENSOR - APPLICATION TO ABITIBI AND KAPUSKASING DATA (CANADA) [J].
CHAKRIDI, R ;
CHOUTEAU, M ;
MARESCHAL, M .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1992, 108 (03) :917-929