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Jökull - 01.01.2010, Qupperneq 60

Jökull - 01.01.2010, Qupperneq 60
Martens et al. 6543210 19 18 17 16 15 14 13 Distance along azimuth 175 [km] D e p th [k m ] 06Jul07 08Jul07 10Jul07 12Jul07 14Jul07 16Jul07 18Jul07 20Jul07 22Jul07 24Jul07 Figure 10. SIL-system 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 293 m. – Upptök jarðskjálfta samkvæmt afstæðum staðsetningum úr SIL-kerfinu og besta nálgun við tvívíðan flöt. Svarta strikalínan sýnir halla flatarins. Horft er eftir strikstefnunni (85◦). Frávik skjálftanna frá fletinum (RMS) er nú 293 m (tafla 2). DISCUSSION It is well known that factors such as network size and station distribution affect the accuracy of hypocen- tre locations (e.g., Bai et al., 2006; Bondár et al., 2004). Table 3 summarises the disparities between the ASN and SIL network sizes and geometrical config- urations. The azimuthal gap provides a quantitative measurement of the extent to which events have oc- curred within the network. Smaller azimuthal gaps indicate denser networks with a preferable geometri- cal configuration. Mean horizontal and vertical absolute location er- rors determined from all 288 single-event locations and as output by HypoInverse-2000 are included for comparison. Consistent with the double-difference relative location uncertainties, ASN single-event er- rors (±0.3 km and ±0.5 km for horizontal and verti- cal errors, respectively) are improved by 40–50% over SIL single-event errors (±0.5 km and ±1.0 km). Sta- tion distribution likely plays the main role as a com- parison of locations based on IMO picks versus our picks for the same six stations yields similar results (i.e., ±0.8 km and ±1.0 km for the horizontal and ver- tical errors, respectively, for the same six stations but different time picks; see also Figure 7). Particularly after relative relocation, SIL does a remarkable job considering the sparseness of the net- work. The orientation of the dyke plane is clear and migration patterns within swarms can be dis- tinguished. One reason for the high quality perfor- mance of the SIL network relative to the denser, local ASN network is that the SIL system is not as sparse 60 JÖKULL No. 60
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