Seismic Hazards Implications of Uplifted Pleistocene Coral Terraces in the Gulf of Aqaba

The Gulf of Aqaba transform plate boundary is a source of destructive teleseismic earthquakes. Seismicity is concentrated in the central sub-basin and decreases to both the north and south. Although principally a strike-slip plate boundary, the faulted margins of the Gulf display largely dip-slip ex...

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Detalles Bibliográficos
Autores principales: Bosworth, W., Montagna, P., Pons-Branchu, E., Rasul, N., Taviani, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5428358/
https://www.ncbi.nlm.nih.gov/pubmed/28232736
http://dx.doi.org/10.1038/s41598-017-00074-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5428358/
https://www.ncbi.nlm.nih.gov/pubmed/28232736
http://dx.doi.org/10.1038/s41598-017-00074-2

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