| PublicID | 2017p341869 |
| UTC Time | 2017-05-07T11:47:53Z |
| Latitude | -41.75 (± 9.2 km) |
| Longitude | 174.19 (± 9.1 km) |
| Depth | 10 km (± 18 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 10 |
| Used Station Count | 10 |
| Standard Error | 0.19 (s) |
| Azimuthal Gap | 120.14 (degrees) |
| Minimum Distance | 0.02 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 2.8 | |
| ML | 3.0 (± 0.2) | 8 |
| MLv | 2.8 (± 0.2) | 8 |
| M | 2.8 | 8 |
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.
