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Magnitude Mw 6.5
Region NEW IRELAND REGION, P.N.G.
Date time 2013-04-23 23:14:46.0 UTC
Location 3.80 S ; 152.18 E
Depth 47 km
Distances 833 km NE of Port Moresby, Papua New Guinea
Event Time
2013-04-24 14:08:57 UTC
2013-04-25 01:08:57 UTC+11:00 at epicenter
2013-04-24 16:08:57 UTC+02:00 system time
Location
18.723°S 169.222°E depth=233.2km (144.9mi)
Nearby Cities
91km (57mi) N of Isangel, Vanuatu
145km (90mi) SE of Port-Vila, Vanuatu
317km (197mi) NE of We, New Caledonia
415km (258mi) SSE of Luganville, Vanuatu
477km (296mi) NE of Dumbea, New Caledonia
GFZ Event gfz2013hykj
13/04/23 23:14:42.91
New Ireland Region, P.N.G.
Epicenter: -3.86 152.09
MW 6.5
GFZ CENTROID MOMENT TENSOR SOLUTION
13/04/23 23:14:41.16
Centroid: -3.8 152.2
Depth 22 No. of sta: 88
Moment Tensor; Scale 10**18 Nm
Mrr= 0.09 Mtt= 6.01
Mpp=-6.10 Mrt=-1.15
Mrp=-1.19 Mtp= 1.26
Principal axes:
T Val= 6.40 Plg=12 Azm=173
N 0.01 75 34
P -6.41 9 265
Best Double Couple:Mo=6.4*10**18
NP1:Strike=309 Dip=75 Slip= 1
NP2: 219 89 165
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I'll review and do a page on eqarchives about this one after the 30 day mark, once things have been processed/reviewed again by CENC, but I wanted to get a handle now on how they operate, so I know how to set up my Excel pages.
New Ireland Region, P.N.G.
Latitude : 2.57 °S
Longitude : 153.86 °E
Depth : 0 Km
Date : 24/04/2013 08:21:32 (UTC)
Magnitude : 4.2 mb
Phase count : 7
April 24, 2013 – GEOLOGY - In the global aftershock zone that followed the major April 2012 Indian Ocean earthquake, seismologists noticed an unusual pattern. The magnitude (M) 8.6 earthquake, a strike-slip event at intra-oceanic tectonic plates, caused global seismic rates of M=4.5 to rise for several days, even at distances thousands of kilometers from the main-shock site. However, the rate of M=6.5 seismic activity subsequently dropped to zero for the next 95 days. This period of quiet, without a large quake, has been a rare event in the past century. So why did this period of quiet occur? In his research presentation, Fred Pollitz of the U.S. Geological Survey suggests that the Indian Ocean earthquake caused short-term dynamic stressing of a global faulting system. Across the planet, there are faults that are “close to failure” and ready to rupture. It may be, suggests Pollitz and his colleagues, that a large quake encourages short-term triggering of these close-to-failure faults but also relieves some of the stress that has built up along these faults. Large magnitude events would not occur until tectonic movement loads stress back on to the faults at the ready-to-fail levels they reached before the main shock. Using a statistical model of global seismicity, Pollitz and his colleagues show that a transient seismic perturbation of the size of the April 2012 global aftershock would inhibit rupture in 88 percent of their possible M=6.5 earthquake fault sources over the next 95 days, regardless of how close they were to failure beforehand. -SD
April 2012 Indian Ocean earthquake.....................However, the rate of M=6.5 seismic activity subsequently dropped to zero for the next 95 days.