What Caused the Recent Earthquakes in the SW Pacific Region?

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Recent seismic activity in the South West Pacific has been notable, with three significant earthquakes recorded: a magnitude 6.5 near Kirakira in the Solomon Islands, a magnitude 6.9 near L'Esperance Rock in the Kermadec Islands, and a magnitude 6.3 near New Caledonia. The discussion also delves into the complexities of analyzing seismic data, particularly when multiple earthquakes occur simultaneously. It highlights the challenge of distinguishing overlapping seismic events on seismographs, especially when aftershocks are closely timed with larger quakes. Experts can often identify these events through advanced techniques, including analyzing P wave arrivals from various sensors in a seismograph network. Filtering techniques, such as high-pass filtering, can enhance the clarity of these signals, making it easier to differentiate between concurrent seismic events.
davenn
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Hi guys

the last 24 hours has seen 3 large quakes in the SW Pacific area

6.5 central Solomon Isl. not far from Kirakira
M 6.5 - 65km NW of Kirakira, Solomon Islands

6.9 southern Kermadec Isl. area
M 6.9 - 61km SW of L'Esperance Rock, New Zealand

6.3 Loyalty Isl area E of New Caledonia
M 6.3 - 202km WNW of Ile Hunter, New Caledonia

the recording from my seismo system
http://www.sydneystormcity.com/seismograms.htm

180909-10  UT M 6.5 Solomons, 6.9 Kermadecs, 6.3 Loyalty Isl zhi.gif
cheers
Dave
 

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@davenn Just a point of clarification for us ignorant types, please. Suppose two unrelated seismic events are concurrent, i.e., overlapping in time. Using the seismic graph, how can you differentiate them?
 
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jim mcnamara said:
Suppose two unrelated seismic events are concurrent, i.e., overlapping in time. Using the seismic graph, how can you differentiate them?

OK this does happen from time to time, actually reasonably regularly.
Mainly with a large event with one or more aftershocks buried in the larger events' signal. I personally haven't been able to see,
say a, M5.5 aftershock that is buried in the M7.2 mainshock if they have occurred within a minute of each other.

here's a recent example ….
Main shock
M 8.2 - 286km NNE of Ndoi Island, Fiji
2018-08-19 00:19:40 (UTC)

Aftershock
M 6.3 - 268km NNE of Ndoi Island, Fiji
2018-08-19 00:23:06 (UTC)

On my recording, I couldn't tell that there were 2 events separated by ~ 4 minutes. But the experts could :smile:

upload_2018-9-12_13-18-4.png
How they do it, I am not sure. Maybe I need to send some emails and see if they will tell me. :biggrin:

Now for the same or closely times events that are separated by some distance, then it becomes easy to differentiate the events using a seismograph network.
as there will always be one or more sensors in the network that are closer to one of those 2 events that what the other sensors are.
It then just becomes a matter of the timing of the P wave arrivals at the various network sensors from which they can then produce locations for the events.hope that helps

Dave
 

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OK with a bit of playing around with filtering. Mainly doing high pass filtering so I could cut out a large portion of the
lower frequency signals. This helps the P wave arrivals from both events to stand out clearer.
I did a 6 pole hi-pass filtered from 1Hz

P arrivals.JPG
 

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