Translated to English from paper in Japanese, originally published in: Memoirs of the Kakioka Magnetic Observatory, Vol.28, No.3 (No.86), pp.1-77, 1989 with permission of the authers.
Geoelectric Observation used by the Telegraphic Facilities of NTT Corporation
Toshio Mori
Contents
-
Introduction
-
Observation method
-
Outline of the observed records
-
Outline of the records at each observation group
-
Comparison of the observed record in the same time of a different day
-
Long-term stability
-
Impedance tensor and transfer function
-
Impedance tensor at the Shimodate group and at Kakioka
-
Impedance tensor at the Mito group and transfer function at Kakioka
-
Time changes of impedance tensors and transfer functions
-
Elimination of the electrical fields induced by geomagnetic variations - Detection of the anomalous earth potential -
-
Analysis method by a stochastic differential equation
-
For geoelectric fields between Kasama and Mito
-
Application to the data of electrical fields at the Mito group and Z at Kakioka
-
Spectral analysis
-
When using per-minute data
-
Use of the transfer function and impedance tensor
-
Relation to tectonic activities
-
Relation to the earthquake swarms off the east coast of the Izu Peninsula
-
Relation to eruptions of Izu-Oshima volcano
-
Other changes
-
Relation to tide, atmospheric pressure and others
-
Application for research of fault structure
-
Iriyama fault
-
Tanna fault
-
Fujikawa fault
-
Anomalous geoelectric change observed near CA (conductivity anomaly) boundary
-
Electrical observation on the sea floor by making use of the power-feeding arrangement of the Permanent Ocean-Bottom Seismograph Observation System off Boso Peninsula (BSOBS)
-
Conclusions
-
Circumstances of observation and acknowledgements
Copyright (c) 1999 Kakioka Magnetic Observatory, Japan Meteorological Agency. All Rights Reserved.