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dc.contributor.author Gu Z.
dc.contributor.author Zhan Z.
dc.contributor.author Gao J.
dc.contributor.author Yao T.
dc.contributor.author Chen B.
dc.date.accessioned 2025-03-15T04:58:38Z
dc.date.available 2025-03-15T04:58:38Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=31339383
dc.identifier.citation Physics and Chemistry of the Earth, Parts A/B/C, 2006, 31, 4-9, 258-267
dc.identifier.issn 1474-7065
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48484
dc.description.abstract During 1993-2002, a field experiment in the Miyun reservoir was carried out. A relation coefficient of -0.063 nT/m was obtained between geomagnetic changes and water depth variations in the reservoir, which agrees with piezomagnetism. The tectonomagnetic investigations suggested static and dynamic tectonomagnetic effects of the active faults. These effects provide useful information for monitoring the potential earthquakes in and near the active faults in the future. The seismomagnetic observation and research in Beijing and its adjacent area show that seismomagnetic precursors are a near-field effect, the anomalous amplitude is 2-11 nT, and the precursor time is several days to one year. These results could be applied in earthquake prediction study. © 2006 Elsevier Ltd. All rights reserved.
dc.subject ACTIVE FAULT
dc.subject BEIJING OF CHINA
dc.subject PIEZOMAGNETIC EXPERIMENT
dc.subject SEISMOMAGNETIC PRECURSOR
dc.subject TECTONOMAGNETIC EFFECT
dc.title SEISMOMAGNETIC RESEARCH IN BEIJING AND ITS ADJACENT AREA, CHINA
dc.type Статья
dc.identifier.doi 10.1016/j.pce.2005.10.002


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