Tectonomagnetic modeling based on the piezomagnetism: a review

Development of tectonomagnetic modeling on the basis of the piezomagnetic effect is reviewed for the period since the early 1990's. First, the basic theory is briefly summarized, in which the representation theorem or the surface integral representation for the piezomagnetic potential and the G...

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Main Author: Y. Sasai
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2001-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3602
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spelling doaj-8b4e763ff7b641c3854d53649148aaf92020-11-25T01:51:57ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2001-06-0144210.4401/ag-3602Tectonomagnetic modeling based on the piezomagnetism: a reviewY. SasaiDevelopment of tectonomagnetic modeling on the basis of the piezomagnetic effect is reviewed for the period since the early 1990's. First, the basic theory is briefly summarized, in which the representation theorem or the surface integral representation for the piezomagnetic potential and the Green's function method are presented. In the 1990's, several field observations in earthquakes and volcanoes were interpreted with the aid of analytic solutions based on the Green's function method. A general formula was developed for an inclined rectangular fault with strike-slip, dip-slip and tensile faulting. The surface integral method has been applied to 2D and 3D models, as well as to fault models in the inhomogeneously magnetized crust. When the magnetic field is measured within a bore hole, the effect of magnetic poles around the hole should be taken into account. As a result, tectonomagnetic signals are much enhanced in a bore hole compared with on the ground surface. Finally, piezomagnetic field changes associated with the Parkfield fault model are introduced and the new aspect of the model is discussed.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3602tectonomagnetic modelingpiezomagnetismseismomagnetic effect of inclined faultenhancement effect of bore holeparkfield fault model
collection DOAJ
language English
format Article
sources DOAJ
author Y. Sasai
spellingShingle Y. Sasai
Tectonomagnetic modeling based on the piezomagnetism: a review
Annals of Geophysics
tectonomagnetic modeling
piezomagnetism
seismomagnetic effect of inclined fault
enhancement effect of bore hole
parkfield fault model
author_facet Y. Sasai
author_sort Y. Sasai
title Tectonomagnetic modeling based on the piezomagnetism: a review
title_short Tectonomagnetic modeling based on the piezomagnetism: a review
title_full Tectonomagnetic modeling based on the piezomagnetism: a review
title_fullStr Tectonomagnetic modeling based on the piezomagnetism: a review
title_full_unstemmed Tectonomagnetic modeling based on the piezomagnetism: a review
title_sort tectonomagnetic modeling based on the piezomagnetism: a review
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2001-06-01
description Development of tectonomagnetic modeling on the basis of the piezomagnetic effect is reviewed for the period since the early 1990's. First, the basic theory is briefly summarized, in which the representation theorem or the surface integral representation for the piezomagnetic potential and the Green's function method are presented. In the 1990's, several field observations in earthquakes and volcanoes were interpreted with the aid of analytic solutions based on the Green's function method. A general formula was developed for an inclined rectangular fault with strike-slip, dip-slip and tensile faulting. The surface integral method has been applied to 2D and 3D models, as well as to fault models in the inhomogeneously magnetized crust. When the magnetic field is measured within a bore hole, the effect of magnetic poles around the hole should be taken into account. As a result, tectonomagnetic signals are much enhanced in a bore hole compared with on the ground surface. Finally, piezomagnetic field changes associated with the Parkfield fault model are introduced and the new aspect of the model is discussed.
topic tectonomagnetic modeling
piezomagnetism
seismomagnetic effect of inclined fault
enhancement effect of bore hole
parkfield fault model
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3602
work_keys_str_mv AT ysasai tectonomagneticmodelingbasedonthepiezomagnetismareview
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