| PublicID | 2014p947498 |
| UTC Time | 2014-12-17T13:47:24Z |
| Latitude | -37.85 (± 38.3 km) |
| Longitude | 179.31 (± 32.4 km) |
| Depth | 38 km (± 26 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 13 |
| Used Station Count | 13 |
| Standard Error | 0.30 (s) |
| Azimuthal Gap | 299.17 (degrees) |
| Minimum Distance | 0.71 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 2.7 | |
| ML | 2.9 (± 0.1) | 8 |
| MLv | 2.7 (± 0.1) | 9 |
| M | 2.7 | 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.