| PublicID | 2016p884162 |
| UTC Time | 2016-11-23T03:21:42Z |
| Latitude | -42.01 (± 2.4 km) |
| Longitude | 173.70 (± 2.7 km) |
| Depth | 10 km (± 3 km) |
| Depth Type | free |
| Earth Model | iasp91 |
| Used Phase Count | 39 |
| Used Station Count | 34 |
| Standard Error | 0.53 (s) |
| Azimuthal Gap | 106.06 (degrees) |
| Minimum Distance | 0.21 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 3.6 | |
| ML | 3.7 (± 0.2) | 17 |
| MLv | 3.6 (± 0.3) | 60 |
| M | 3.6 | 60 |
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.