| PublicID | 2012p007258 |
| UTC Time | 2012-01-03T16:27:05Z |
| Latitude | -43.43 (± 1.6 km) |
| Longitude | 172.81 (± 2.5 km) |
| Depth | 5 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | iasp91 |
| Used Phase Count | 23 |
| Used Station Count | 16 |
| Standard Error | 0.51 (s) |
| Azimuthal Gap | 135.09 (degrees) |
| Minimum Distance | 0.12 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (ML) | 4.0 (± 0.3) | |
| ML | 4.0 (± 0.3) | 57 |
| MLh | 4.2 (± 0.5) | 4 |
| MLv | 3.6 (± 0.5) | 5 |
| Mjma | 3.5 (± 0.4) | 5 |
| M | 3.6 | 5 |
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.