Determination of the Fault Plane for the 2007 Kuril Islands Earthquake using the Hypocenter Relocations of Aftershocks.
Two great earthquakes occurred in the Kuril Islands region in 2006 and
2007. The Kuril Islands earthquake of the 15 Nobember 2006 (Mw 8.3)
occurred on the boundary between the Pacific Plate and Okhotsk Plate.
About only two months later, a Mw 8.1 earthquake on 13 January 2007,
occurred with an epicentre approximately 95 km ESE of the November
earthquake, close to the outer-rise portion of the Pacific Plate.
It is relatively-uncommon that great earthquakes (Mw > 8.0) have
occurred in the same region within a short span of the time, also great
outer-rise earthquakes (Mw > 8.0) have occurred only three times since
the early 20th century.
The aim of this study is estimate the orientation of the fault plane for
the 2007 outer-rise earthquake. It is reasonable to assume that the
fault plane of the 2006 earthquake is on the northwest dipping
subduction plate boundary, however, there is currently not a clear
indication of the geometry of the 2007 earthquake.
To relocate the associated seismicity, we used well recorded master
events. The depth of the master event was determined by teleseismic
waveform modelling, using the programme of Kikuchi and Kanamori, 2003.
To relocate the seismicity we used the location programme HYPOCENTER 3.2
[Lienert, 1994]. For the master events, the earthquake were relocated
with the depth was fixed at the value determined from a waveform
inversions. The station residuals from the master event relocations were
subtracted from the arrival times of the other events and the events
were relocated. The data we used are P wave arrival time data compiled
by the United States Geological Survey (USGS) during the period 20
September 2006 to 15 March 2007. Number of earthquakes were 1651.
The results of relative relocations show that the fault plane of the
2006 thrust event is a shallowly northwest dipping plane and the 2007
normal fault event is dipping more steeply to the southeast.