PublicID | 2024p897079 |
UTC Time | 2024-11-27T22:03:59Z |
Latitude | -37.68 (± 4.2 km) |
Longitude | 179.68 (± 4.3 km) |
Depth | 33 km (± 0 km) |
Depth Type | operator assigned |
Earth Model | iasp91 |
Used Phase Count | 47 |
Used Station Count | 35 |
Standard Error | 0.90 (s) |
Azimuthal Gap | 136.16 (degrees) |
Minimum Distance | 0.89 (degrees) |
Type | Magnitude | Station Count |
Preferred (M) | 5.9 | |
mB | 6.2 (± 0.1) | 7 |
Mw(mB) | 5.9 (± 0.4) | 7 |
ML | 5.7 (± 0.2) | 17 |
MLv | 5.8 (± 0.2) | 60 |
M | 5.9 | 60 |
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.