A magnetotelluric study of the Alpine Fault, New Zealand

被引:18
|
作者
Ingham, M
Brown, C
机构
[1] Victoria Univ Wellington, Inst Geophys, Wellington, New Zealand
[2] Univ Coll Galway, Appl Geophys Unit, Galway, Ireland
关键词
Alpine Fault; magnetotelluric sounding; resistivity;
D O I
10.1046/j.1365-246X.1998.00659.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
Magnetotelluric soundings have been made at seven locations on a 4 km profile crossing the Alpine Fault in the South Island of New Zealand. The 'distortion' techniques of Groom & Bailey (1989) and Lilley (1998 a,b) have been used to derive regional apparent resistivity and phase curves that correspond to electromagnetic induction in orientations parallel and perpendicular to the fault. 2-D inversion of the regional responses reveals that a narrow (<1 km wide) conductive zone is associated with the Alpine Fault. This conductor is most probably related to the heating of deep circulating meteoric water in a region in which enhanced temperatures occur at shallow depth due to the tectonic uplift of the Southern Alps.
引用
收藏
页码:542 / 552
页数:11
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