| PublicID | 2017p100432 |
| UTC Time | 2017-02-07T03:50:10Z |
| Latitude | -41.17 (± 24.3 km) |
| Longitude | 174.44 (± 31.3 km) |
| Depth | 277 km (± 26 km) |
| Depth Type | free |
| Earth Model | iasp91 |
| Used Phase Count | 12 |
| Used Station Count | 9 |
| Standard Error | 6.06 (s) |
| Azimuthal Gap | 322.00 (degrees) |
| Minimum Distance | 1.88 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 3.8 | |
| ML | 4.1 (± 0.3) | 5 |
| MLv | 3.8 (± 0.1) | 7 |
| M | 3.8 | 7 |
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.