| PublicID | 2020p107455 |
| UTC Time | 2020-02-09T18:12:21Z |
| Latitude | -45.27 (± 4.4 km) |
| Longitude | 167.08 (± 6.6 km) |
| Depth | 26 km (± 6 km) |
| Depth Type | free |
| Earth Model | iasp91 |
| Used Phase Count | 24 |
| Used Station Count | 18 |
| Standard Error | 0.49 (s) |
| Azimuthal Gap | 208.31 (degrees) |
| Minimum Distance | 0.20 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 3.7 | |
| MLv | 3.7 (± 0.3) | 12 |
| ML | 3.3 (± 0.3) | 9 |
| M | 3.7 | 12 |
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.
