| PublicID | 2018p691168 |
| UTC Time | 2018-09-13T17:34:10Z |
| Latitude | -34.85 (± 5.4 km) |
| Longitude | -178.92 (± 10.2 km) |
| Depth | 102 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | iasp91 |
| Used Phase Count | 65 |
| Used Station Count | 45 |
| Standard Error | 1.55 (s) |
| Azimuthal Gap | 200.81 (degrees) |
| Minimum Distance | 3.86 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (M) | 4.9 | |
| ML | 5.7 (± 0.1) | 7 |
| MLv | 5.3 (± 0.1) | 32 |
| mB | 5.4 (± 0.1) | 17 |
| Mw(mB) | 4.8 (± 0.4) | 17 |
| M | 4.9 | 32 |
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.