Localisation of Earthquakes and their Tracking in Real-time
Some Basic Elements for possible Incorporation into Earthquake Early Warning (EEWS) Systems
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Having previously worked on locating micro-seismic events within Cornish Batholiths at a Geothermal Energy Project (¿Hot Dry Rocks¿) in Cornwall, England in the 1980¿s, attention became focused on further, and larger work, by the occurrence of the Tsunami in 2004 and the large Earthquakes in Sichuan (China, 2008). Algorithms have been devised that may run in real-time, acting as initial stages in the response of EEW Systems. These algorithms consider both the assumed spherical and the spheroidal Earth geometry, directly, and can deliver the Epicenter and Hypocenter for each event concurrent...
Having previously worked on locating micro-seismic events within Cornish Batholiths at a Geothermal Energy Project (¿Hot Dry Rocks¿) in Cornwall, England in the 1980¿s, attention became focused on further, and larger work, by the occurrence of the Tsunami in 2004 and the large Earthquakes in Sichuan (China, 2008). Algorithms have been devised that may run in real-time, acting as initial stages in the response of EEW Systems. These algorithms consider both the assumed spherical and the spheroidal Earth geometry, directly, and can deliver the Epicenter and Hypocenter for each event concurrently, using tabular scanning methods. The algorithms developed here were tested against a catalogue of seven Earthquakes, of mixed depth and magnitude, whose data was selected from Databases held by IRIS (Incorporated Research Institutes for Seismology). It is considered that this text might be considered as an initial source for anybody about to design software for their own seismic observatory
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