Jökull


Jökull - 01.01.2010, Page 61

Jökull - 01.01.2010, Page 61
Upptyppingar seismic swarms 6543210 19 18 17 16 15 14 13 Distance along azimuth 165 [km] D e p th [k m ] 06Jul07 08Jul07 10Jul07 12Jul07 14Jul07 16Jul07 18Jul07 20Jul07 22Jul07 24Jul07 Figure 11. ASN double-difference relative locations fit to a plane using linear regression. A dashed, black line depicts the best-fit plane and the view is looking along the strike direction (Table 2). The RMS misfit to the plane is 135 m (or 114 m if the two off-axis points between 16.5 and 17.0 km are removed). Here the orien- tation of the plane (075/49) is well defined owing to the precise alignment of the hypocentres. – Besta nálgun við tvívíðan flöt samkvæmt afstæðum staðsetningum úr ASN mælanetinu. Svört strikalína sýnir halla flatarins, horft er eftir strikstefnunni (tafla 2). Ferningsmeðaltal (RMS) fráviks við flötinn er 135 m (eða 114 m ef tveimur fjarlægum punktum á 16,5 og 17,0 km dýpi er sleppt). Flöturinn er vel skilgreindur með strikstefnu 75◦ og halla 49◦. Table 3. Station coverage and absolute location uncertainties for the 6–24 July 2007 events de- rived from SIL and ASN single-event locations in HypoInverse-2000. – Afstaða stöðva og óvissa í afstæðum staðsetningum jarðskjálfta á tímabilinu 6.–24. júlí samkvæmt SIL-kerfinu og ASN netinu. SIL ASN Mean Azimuthal Gap (◦) 135 82 Mean Distance to Nearest Station (km) 5.9 2.6 Mean Number of P/S Picks 16 42 Mean Absolute Horizontal Error (km) 0.5 0.3 Mean Absolute Vertical Error (km) 1.0 0.5 in the Upptyppingar area as in most regions of Ice- land. This is due to the fortuitous installation of six nearby stations in 2004 to monitor the formation of the Hálslón water reservoir (Jakobsdóttir, 2008). All six SIL stations lie within 30 km of the Upptypping- ar events. Moreover, SIL network stations are de- ployed in vaults whereas most of the Cambridge Uni- versity instruments, intended for temporary deploy- ment, were buried directly in sand, dirt and pumice. The SIL method of deployment reduces noise levels in the seismic signals, which allows for more precise time picking and locations. JÖKULL No. 60 61
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