PublicID | 2020p637922 |
UTC Time | 2020-08-24T00:45:12Z |
Latitude | -29.02 (± 5.0 km) |
Longitude | -176.61 (± 5.4 km) |
Depth | 12 km (± 0 km) |
Depth Type | operator assigned |
Earth Model | iasp91 |
Used Phase Count | 25 |
Used Station Count | 20 |
Standard Error | 1.06 (s) |
Azimuthal Gap | 146.90 (degrees) |
Minimum Distance | 1.17 (degrees) |
Type | Magnitude | Station Count |
Preferred (mB) | 5.4 (± 0.2) | |
ML | 6.2 (± 0.2) | 2 |
MLv | 6.1 (± 0.1) | 2 |
mB | 5.4 (± 0.2) | 6 |
Mw(mB) | 4.9 (± 0.4) | 6 |
M | 5.6 | 6 |
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.