Improved seismic data and computer facilities have made dramatic progress possible in the computational techniques of earthquake location and the quantification of earthquakes. Some of the more proven techniques may well be ready for application in the routine reporting of earthquake parameters. Earthquake parameters serve as an important data base for the generalists and synthesizers in seismology and as an initial starting point for the applied theoreticians. The routine determination and reporting of source properties, for example, could make possible a new level of understanding in many seismological studies that would parallel the use of routinely reported earthquake locations to define boundaries of tectonic plates worldw...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...
Physically justified choice of seismological parameters for seismic situation monitoring directed to...
Our current understanding of the Earth’s interior structure and processes is limited to observations...
Studying seismograms is the first step in the scientific study of earthquakes and the interior of th...
The difficulties of locating earthquakes in the early instrumental period are not always fully appre...
An electronic digital computer program has been developed for determining the source and origin time...
In this exercise, students use data from the 1994 Northridge, California, earthquake to locate the e...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1979.M...
A program for the location of hypocenters of local shocks by means of an electronic digital computer...
Recordings of earthquakes were used to calculate the magnification of ground motion produced by vari...
An explanation of methods used to determine instrumentally the exact epicentre of an earthquake, als...
The first part of this study describes a technique by which the source parameters of an earthquake c...
Accurate earthquake locations are crucial for investigating seismogenic processes, as well as for ap...
Earthquakes affected mankind since the days of old, claiming more human casualties than any other na...
Earthquake locations are fundamental to studies of earthquake physics, fault orientations and Earth'...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...
Physically justified choice of seismological parameters for seismic situation monitoring directed to...
Our current understanding of the Earth’s interior structure and processes is limited to observations...
Studying seismograms is the first step in the scientific study of earthquakes and the interior of th...
The difficulties of locating earthquakes in the early instrumental period are not always fully appre...
An electronic digital computer program has been developed for determining the source and origin time...
In this exercise, students use data from the 1994 Northridge, California, earthquake to locate the e...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1979.M...
A program for the location of hypocenters of local shocks by means of an electronic digital computer...
Recordings of earthquakes were used to calculate the magnification of ground motion produced by vari...
An explanation of methods used to determine instrumentally the exact epicentre of an earthquake, als...
The first part of this study describes a technique by which the source parameters of an earthquake c...
Accurate earthquake locations are crucial for investigating seismogenic processes, as well as for ap...
Earthquakes affected mankind since the days of old, claiming more human casualties than any other na...
Earthquake locations are fundamental to studies of earthquake physics, fault orientations and Earth'...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...
Physically justified choice of seismological parameters for seismic situation monitoring directed to...
Our current understanding of the Earth’s interior structure and processes is limited to observations...