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Origin
PublicID |
2018p044238 |
UTC Time |
2018-01-17T08:50:07Z |
Latitude |
-45.24 (± 26.7
km)
|
Longitude |
167.05 (± 42.2
km)
|
Depth |
15 km (± 35 km) |
Depth Type |
free |
Earth Model |
nz3drx |
Used Phase Count |
10 |
Used Station Count |
10 |
Standard Error |
1.00 (s) |
Azimuthal Gap |
213.63 (degrees) |
Minimum Distance |
0.25 (degrees) |
Magnitudes
Type |
Magnitude |
Station Count |
Preferred (M) |
2.8 |
|
ML |
2.8 (± 0.4) |
5 |
MLv |
2.8 (± 0.1) |
2 |
M |
2.8 |
2 |
GeoNet combines magnitudes into a summary magnitude, M, which consists of a weighted average of the individual magnitudes and attempts to be a best possible compromise between all magnitudes for a range of earthquake sizes.
Summary magnitude for GeoNet is then defined as:
M = (2 * MLv + (0.4 * number_of stations(Mw(mB)) - 1) * Mw(mB)) / (2 + (0.4 * number_of_stations(Mw(mB)) - 1))
Where MLv is local magnitude calculated on the vertical component and Mw(mB) is a Mw estimation based of mB by Bormann and Saul (2008).