| PublicID | 2023p039206 |
| UTC Time | 2023-01-15T12:09:10Z |
| Latitude | -36.56 (± 29.4 km) |
| Longitude | 175.10 (± 34.4 km) |
| Depth | 59 km (± 49 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 10 |
| Used Station Count | 10 |
| Standard Error | 1.06 (s) |
| Azimuthal Gap | 143.30 (degrees) |
| Minimum Distance | 0.22 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 2.8 | |
| MLv | 2.8 (± 0.5) | 8 |
| M | 2.8 | 8 |
| ML | 2.1 (± 0.6) | 8 |
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.
