| PublicID | 2016p858601 |
| UTC Time | 2016-11-13T16:22:48Z |
| Latitude | -39.31 (± 20.8 km) |
| Longitude | 176.20 (± 18.4 km) |
| Depth | 25 km (± 23 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 21 |
| Used Station Count | 21 |
| Standard Error | 1.44 (s) |
| Azimuthal Gap | 160.84 (degrees) |
| Minimum Distance | 0.40 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 3.0 | |
| MLv | 3.0 (± 0.1) | 15 |
| M | 3.0 | 15 |
| ML | 3.2 (± 0.2) | 9 |
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.