PublicID | 2022p771854 |
UTC Time | 2022-10-13T14:03:56Z |
Latitude | -40.39 (± 4.0 km) |
Longitude | 173.43 (± 6.9 km) |
Depth | 146 km (± 9 km) |
Depth Type | free |
Earth Model | iasp91 |
Used Phase Count | 32 |
Used Station Count | 26 |
Standard Error | 0.36 (s) |
Azimuthal Gap | 139.78 (degrees) |
Minimum Distance | 0.56 (degrees) |
Type | Magnitude | Station Count |
Preferred (MLv) | 5.7 (± 0.2) | |
M | 5.7 | 49 |
Mw(mB) | 5.6 (± 0.4) | 7 |
MLv | 5.7 (± 0.2) | 49 |
mB | 6.0 (± 0.2) | 9 |
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).
Map showing stations with picks used to locate the earthquake. Stations with picks that have a zero weight in the solution are shown as small grey circles. Those with a higher weight are shown as larger circles. The quake is shown by the largest circle.