PublicID | 2024p140653 |
UTC Time | 2024-02-22T01:00:06Z |
Latitude | -41.05 (± 3.5 km) |
Longitude | 175.52 (± 5.7 km) |
Depth | 15 km (± 8 km) |
Depth Type | free |
Earth Model | iasp91 |
Used Phase Count | 11 |
Used Station Count | 9 |
Standard Error | 0.09 (s) |
Azimuthal Gap | 94.57 (degrees) |
Minimum Distance | 0.11 (degrees) |
Type | Magnitude | Station Count |
Preferred (MLv) | 1.1 (± 0.3) | |
MLv | 1.1 (± 0.3) | 3 |
ML | 1.0 (± 0.1) | 6 |
M | 1.1 | 3 |
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.