PublicID | 2022p036547 |
UTC Time | 2022-01-14T12:31:23Z |
Latitude | -33.01 (± 28.1 km) |
Longitude | -179.66 (± 30.8 km) |
Depth | 350 km (± 58 km) |
Depth Type | free |
Earth Model | iasp91 |
Used Phase Count | 23 |
Used Station Count | 16 |
Standard Error | 0.73 (s) |
Azimuthal Gap | 332.33 (degrees) |
Minimum Distance | 5.05 (degrees) |
Type | Magnitude | Station Count |
Preferred (MLv) | 4.2 (± 0.4) | |
MLv | 4.2 (± 0.4) | 3 |
ML | 3.9 (± 0.1) | 12 |
mB | 4.4 (± 0.3) | 5 |
Mw(mB) | 3.5 (± 0.4) | 5 |
M | 4.0 | 5 |
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.