| PublicID | 2013p564359 |
| UTC Time | 2013-07-28T19:30:51Z |
| Latitude | -41.66 (± 1.6 km) |
| Longitude | 174.27 (± 1.4 km) |
| Depth | 11 km (± 3 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 33 |
| Used Station Count | 29 |
| Standard Error | 0.33 (s) |
| Azimuthal Gap | 123.85 (degrees) |
| Minimum Distance | 0.10 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 2.8 | |
| MLv | 2.8 (± 0.3) | 25 |
| ML | 3.1 (± 0.1) | 20 |
| M | 2.8 | 25 |
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.