Effect of glacial-interglacial sea-level changes on the displacement and stress field in the forearc and along the plate interface of subduction zones
Combined seismological, space-geodetic and numerical studies have shown that the seismicity at subduction zones may be modulated by tides and glacier fluctuations on timescales of 1-100 a, because these changes in loads on Earth's surface are able to alter the stress field in the upper plate an...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Göttingen : Copernicus GmbH
2012
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Online Access: | https://dx.doi.org/10.15488/1088 http://www.repo.uni-hannover.de/handle/123456789/1112 |