PublicID | 2024p333332 |
UTC Time | 2024-05-03T07:59:28Z |
Latitude | -45.41 (± 3.4 km) |
Longitude | 166.99 (± 4.3 km) |
Depth | 51 km (± 6 km) |
Depth Type | free |
Earth Model | iasp91 |
Used Phase Count | 31 |
Used Station Count | 17 |
Standard Error | 0.57 (s) |
Azimuthal Gap | 130.68 (degrees) |
Minimum Distance | 0.12 (degrees) |
Type | Magnitude | Station Count |
Preferred (MLv) | 5.1 (± 0.2) | |
mB | 5.1 (± 0.2) | 29 |
ML | 4.8 (± 0.2) | 9 |
MLv | 5.1 (± 0.2) | 21 |
Mw(mB) | 4.4 (± 0.4) | 29 |
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.