Spatiotemporal distribution of the seismicity along the Mid-Atlantic Ridge north of the Azores from hydroacoustic data: Insights into seismogenic processes in a ridge-hot spot context

The seismicity of the North Atlantic was monitored from May 2002 to September 2003 by the 'SIRENA array' of autonomous hydrophones. The hydroacoustic signals provide a unique data set documenting numerous low-magnitude earthquakes along the section of the Mid-Atlantic Ridge (MAR) located i...

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Detalhes bibliográficos
Autor principal: Goslin, J. (author)
Outros Autores: Perrot, J. (author), Royer, J. -Y. (author), Martin, C. (author), Lourenco, N. (author), Luis, J. (author), Dziak, R. P. (author), Matsumoto, H. (author), Haxel, J. (author), Fowler, M. J. (author), Fox, C. G. (author), Lau, A. T. -K. (author), Bazin, S. (author)
Formato: article
Idioma:eng
Publicado em: 2018
Assuntos:
Hydrophone arrays
Reykjanes ridge
Midocean ridges
Omori formula
Sea-floor
T-waves
Gravity
Earthquakes
Evolution
Segmentation
Texto completo:http://hdl.handle.net/10400.1/11327
País:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/11327

Texto Completo

http://hdl.handle.net/10400.1/11327

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