The electric field mill in our underground observation room detected a co-seismic electromagnetic signal in the vertical electrostatic field ca. 8 s after the origin time of the Niigataken Chuetsu-oki Earthquake in 2007, but ca. 30 s before the arrival time of the P-waves.
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Kan OKUBO, Akihiro TAKEUCHI, Yukinobu NAKAMURA, Nobunao TAKEUCHI, "Underground Electric Signal at the Occurrence of the Niigataken Chuetsu-oki Earthquake in 2007, Japan" in IEICE TRANSACTIONS on Electronics,
vol. E95-C, no. 1, pp. 110-114, January 2012, doi: 10.1587/transele.E95.C.110.
Abstract: The electric field mill in our underground observation room detected a co-seismic electromagnetic signal in the vertical electrostatic field ca. 8 s after the origin time of the Niigataken Chuetsu-oki Earthquake in 2007, but ca. 30 s before the arrival time of the P-waves.
URL: https://global.ieice.org/en_transactions/electronics/10.1587/transele.E95.C.110/_p
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@ARTICLE{e95-c_1_110,
author={Kan OKUBO, Akihiro TAKEUCHI, Yukinobu NAKAMURA, Nobunao TAKEUCHI, },
journal={IEICE TRANSACTIONS on Electronics},
title={Underground Electric Signal at the Occurrence of the Niigataken Chuetsu-oki Earthquake in 2007, Japan},
year={2012},
volume={E95-C},
number={1},
pages={110-114},
abstract={The electric field mill in our underground observation room detected a co-seismic electromagnetic signal in the vertical electrostatic field ca. 8 s after the origin time of the Niigataken Chuetsu-oki Earthquake in 2007, but ca. 30 s before the arrival time of the P-waves.},
keywords={},
doi={10.1587/transele.E95.C.110},
ISSN={1745-1353},
month={January},}
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TY - JOUR
TI - Underground Electric Signal at the Occurrence of the Niigataken Chuetsu-oki Earthquake in 2007, Japan
T2 - IEICE TRANSACTIONS on Electronics
SP - 110
EP - 114
AU - Kan OKUBO
AU - Akihiro TAKEUCHI
AU - Yukinobu NAKAMURA
AU - Nobunao TAKEUCHI
PY - 2012
DO - 10.1587/transele.E95.C.110
JO - IEICE TRANSACTIONS on Electronics
SN - 1745-1353
VL - E95-C
IS - 1
JA - IEICE TRANSACTIONS on Electronics
Y1 - January 2012
AB - The electric field mill in our underground observation room detected a co-seismic electromagnetic signal in the vertical electrostatic field ca. 8 s after the origin time of the Niigataken Chuetsu-oki Earthquake in 2007, but ca. 30 s before the arrival time of the P-waves.
ER -