Preliminary Analysis of the 21 February 2008 Svalbard (Norway) Seismic Sequence

• DOI: 10.1785/gssrl.81.1.63
• Publication Date: 2010-01-05T23:48:05Z
• Authors: M. Pirli; J. Schweitzer; L. Ottemoller; M. Raeesi; R. Mjelde; K. Atakan; A. Guterch; S. J. Gibbons; B. Paulsen; W. Debski; P. Wiejacz; T. Kvaerna
• Keywords: 13. Climate action; 14. Life underwater; 01 natural sciences; 0105 earth and related environmental sciences

Research Article| January 01, 2010 Preliminary Analysis of the 21 February 2008 Svalbard (Norway) Seismic Sequence Myrto Pirli; Pirli NORSAR PO Box 53 N-2027, Kjeller Norway [e-mail] (M. P.) 1Norwegian Array (NORSAR), Kjeller, Search for other works by this author on: GSW Google Scholar Johannes Schweitzer; Schweitzer Lars Ottemöller; Ottemöller 2British Geological Survey, Edinburgh, Scotland, U.K.; now at University Bergen, Department Earth Sciences. Mohammad Raeesi; Raeesi 3Department Sciences, Rolf Mjelde; Mjelde Kuvvet Atakan; Atakan Aleksander Guterch; Guterch 4Institute Geophysics, Polish Academy Warsaw, Poland Steven J. Gibbons; Gibbons Berit Paulsen; Paulsen Wojciech Dębski; Dębski Paweł Wiejacz; Wiejacz Tormod Kværna Author and Article Information Publisher: Seismological Society America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print 0895-0695 © Letters (2010) 81 (1): 63–75. https://doi.org/10.1785/gssrl.81.1.63 history Cite View This Citation Add to Manager Share Icon Facebook Twitter LinkedIn MailTo Tools Get Permissions Site Pirli, Schweitzer, Ottemöller, Raeesi, Mjelde, Atakan, Guterch, Gibbons, Paulsen, Dębski, Wiejacz, Kværna; Sequence. 2010;; doi: Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Dropdown Menu input auto suggest filter your All ContentBy SocietySeismological Advanced The Archipelago is situated in northwestern part Barents shelf, close proximity passive continental margin. intraplate region characterized some highest seismicity entire Sea adjoining surpassed only Knipovich ridge (e.g., Engen et al. 2003; International Centre 2001), which, as a spreading plate boundary, structure that dominates regional stress field. Most seismic activity (Figure 1) smaller events, which often occur small concentrations sparsely distributed time. However,... You do not have access content, please speak institutional administrator if you feel should access.