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This small volume aims to suggest and demonstrate a collection of methods whereby very rapid scans for the Hypocenter foci can take place in real-time or near real-time. These scans have been, to some extent, given in other places and are to be executed, in part, by point-to-point (P2P) ray-tracers or Tabular Scans. These ray tracers act from a set of depth-points from which the scan constructs rays to each of the active seismographs which are in possession of a P-wave or S-wave onset timing. The P2P tracers employ any of a set of 1-D (radial) Earth velocity models and use a set of possible…mehr

Produktbeschreibung
This small volume aims to suggest and demonstrate a collection of methods whereby very rapid scans for the Hypocenter foci can take place in real-time or near real-time. These scans have been, to some extent, given in other places and are to be executed, in part, by point-to-point (P2P) ray-tracers or Tabular Scans. These ray tracers act from a set of depth-points from which the scan constructs rays to each of the active seismographs which are in possession of a P-wave or S-wave onset timing. The P2P tracers employ any of a set of 1-D (radial) Earth velocity models and use a set of possible "indicator functions" whose response shall determine an estimate of the Hypocenter Depth.
Autorenporträt
G. Daglish traveled in Norway and N. Nigeria,graduated at the Open University (England,1982) and gained a Doctorate in Mathematics at Birkbeck College (London,1992). Yu. Sizov graduated from the Kazan State University, gained a Doctorate in Natural Sciences at the Russian Academy and worked at the Pushkov Institute on terrestrial electro-magnetism.