Select a format below to download the complete technical data for this earthquake. [Succinct microcopy that describes what QUAKEML and STRONG is and that the open data in the current tab and do not download a file and that shaking layers is on an external site]
Calculated source location of the earthquake. It contains the parameters GeoNet's location software derived from seismic station observations.
| PublicID | 2012p340490 |
| UTC Time | 2012-05-05T23:33:13Z |
| Latitude | -41.39 (± 1.4 km) |
| Longitude | 174.67 (± 1.1 km) |
| Depth | 28 km (± 1 km) |
| Depth Type | free |
| Earth Model | nz3drx |
| Used Phase Count | 29 |
| Used Station Count | 20 |
| Standard Error | 0.18 (s) |
| Azimuthal Gap | 111.67 (degrees) |
| Minimum Distance | 0.12 (degrees) |
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.
| Type | Magnitude | Station Count |
|---|---|---|
| Preferred (M) | 4.1 | |
| MLv | 4.1 (± 0.3) | 99 |
| ML | 4.4 (± 0.2) | 7 |
| M | 4.1 | 99 |
| Minimum distance | 0.12 (degree) |
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).
Observed arrival time at a seismic station compared to a predicted arrival time from a GeoNet waveform propagation model (a given velocity model (1D or 3D)). A residual of 0 s indicates that the observed seismic phase arrival time (typically P or S) matches the arrival time predicted by the GeoNet velocity model. Low residuals across multiple well-distributed stations increase confidence in the estimated event location and origin time. Large (brown) points are used to determine the current solution, small (grey) points are observations not used.
MLv is the local (Richter) magnitude computed from amplitudes measured on the vertical component.
The individual magnitude estimates calculated from each seismic station using the ML (Local Magnitude) method. ML is the standard local (Richter) magnitude computed from amplitudes measured on the horizontal component, originally designed for Southern California by Richter (1935).
How much the magnitude calculated at an individual station differs from the average magnitude. A negative residual means the station magnitude is lower than the average magnitude, and a positive residual means it's higher. MLv is the local (Richter) magnitude computed from amplitudes measured on the vertical component. Large (brown) points are used to determine the current solution, small (grey) points are observations not used.
How much the magnitude calculated at an individual station differs from the average magnitude. A negative residual means the station magnitude is lower than the average magnitude, and a positive residual means it's higher. ML is the local (Richter) magnitude computed from amplitudes measured on the horizontal component. Large (brown) points are used to determine the current solution, small (grey) points are observations not used.
