PublicID | 2020p055829 |
UTC Time | 2020-01-21T15:40:23Z |
Latitude | -26.78 (± 10.6 km) |
Longitude | -173.97 (± 15.5 km) |
Depth | 100 km (± 0 km) |
Depth Type | operator assigned |
Earth Model | iasp91 |
Used Phase Count | 12 |
Used Station Count | 10 |
Standard Error | 1.91 (s) |
Azimuthal Gap | 181.45 (degrees) |
Minimum Distance | 4.28 (degrees) |
Type | Magnitude | Station Count |
Preferred (mB) | 4.8 (± 0.3) | |
MLv | 5.1 | 1 |
mB | 4.8 (± 0.3) | 3 |
Mw(mB) | 4.0 (± 0.4) | 3 |
M | 5.0 | 3 |
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.