PublicID | 2022p431491 |
UTC Time | 2022-06-09T15:38:01Z |
Latitude | -31.98 (± 19.7 km) |
Longitude | 179.80 (± 49.0 km) |
Depth | 249 km (± 29 km) |
Depth Type | free |
Earth Model | iasp91 |
Used Phase Count | 18 |
Used Station Count | 11 |
Standard Error | 0.92 (s) |
Azimuthal Gap | 196.51 (degrees) |
Minimum Distance | 3.34 (degrees) |
Type | Magnitude | Station Count |
Preferred (mB) | 4.7 | |
MLv | 4.4 (± 0.4) | 5 |
ML | 4.3 (± 0.1) | 3 |
mB | 4.7 | 1 |
Mw(mB) | 3.9 (± 0.4) | 1 |
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.