Microearthquakes preceding a M4.2 Earthquake Offshore Istanbul

A primary hurdle in observing small foreshocks is the detection-limit of most seismic networks, which is typically about magnitude M1-1.5. We show that a start-up test of a borehole-based seismic network with a much lower detection limit overcame this problem for an M(w)4.2 earthquake. This earthqua...

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Detalles Bibliográficos
Autores principales: Malin, Peter E., Bohnhoff, Marco, Blümle, Felix, Dresen, Georg, Martínez-Garzón, Patricia, Nurlu, Murat, Ceken, Ulubey, Kadirioglu, Filiz Tuba, Kartal, Recai Feyiz, Kilic, Tugbay, Yanik, Kenan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6212396/
https://www.ncbi.nlm.nih.gov/pubmed/30385791
http://dx.doi.org/10.1038/s41598-018-34563-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6212396/
https://www.ncbi.nlm.nih.gov/pubmed/30385791
http://dx.doi.org/10.1038/s41598-018-34563-9

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