Jökull


Jökull - 01.01.2010, Page 81

Jökull - 01.01.2010, Page 81
Intraplate earthquake swarms in Central Europe The plot of the areal density of the IA (Figure 10a) clearly evidenced that vast majority of immediate af- tershocks was located close to prior events. Hence, we estimated the areal density of the immediate af- tershocks as a function of normalized distance from the centre of the PEs to find out whether the after- shocks were generated preferably near the edge of the PE rupture. As it is apparent from Figure 10b, the IA density increases from a small value within the rup- ture area to a narrow maximum at distances between 1 and 2 PE radii; at greater distances the density rapidly decreases. The areal density for 5th and 50th after- shocks shows similar trend; however, it shows much smaller maximum in both cases. These results ap- parently point out triggering effect of the prior events upon the subsequent ones and signify prevailing ori- gin of aftershocks close to the edge of the PE rupture. Inter-event-times in the 2000 swarm, which range from less than 1s up to more than 104 s, indicate vari- ous speed of interaction between prior and subsequent events: about, 40% and 8% of the ML>0.5 IAs were linked with the PEs by velocities above 10 m/s and 100 m/s, respectively. We examined the PE – IA in- teractions in term of their rapidity and preferential oc- currence directions. To this purpose we calculated the number of the IAs in the angular sectors of 10◦ on the whole fault plane for different intervals of inter-event velocities. The resulting IA-rate polar plots for all the ML>0.5 IAs, and for inter-event velocities higher than 10 m/s and 100 m/s are depicted in Figure 11. All three plots show a distinct prevalence of the IA occur- rence along the direction of 30◦ to 40◦ from horizontal plane which corresponds to the slip-parallel direction revealed by the retrieved source mechanisms. The po- 0 1 2 3 4 5 6 7 8 9 10 0 5 10 15 20 25 30 35 40 45 Normalized aftershock distance 5th IA Areal density of aftershocks per unit rupture area 50th a) b) Figure 10. Areal density of positions of immediate aftershocks (IAs) relative to the position of previous events (PEs); the coordinates are projected on a common fault plane. Density plot in a) shows the number of events per 100 m2; in b) the coordinates of IAs are normalized by nominal radius of PEs defined as R=30 x 100.35ML , and the areal density of 1st, 5th and 50th aftershock is shown. – Þéttleiki staðsetninga eftirskjálfta miðað við staðsetningu skjálftans á undan. Hnitunum er varpað á sameiginlegan brotflöt. Myndin til vinstri sýnir fjölda skjálfta fyrir hverja 100 m2. Myndin til hægri sýnir fjarlægð eftirskjálfta eftir stöðlun með mati á stærð skjálftans, R=30 x 100.35ML . Myndin sýnir þéttleikann fyrir fyrsta, fimmta og fimmtugasta eftirskjálftann. JÖKULL No. 60 81
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