This paper is in continuation of previous investigations (Gutenberg<br />and Richter, Paper I, 1942; Paper I I , 1956).<br />The earthquake magnitude has statistical and other uses independent<br />of the relation between magnitude and energy. Indeed, it is possible<br />that there is no complete one-to-one correlation between magnitude<br />and energy for large and complex tectonic events. Even so, a<br />mean or representative relation is a legitimate object of inquiry
Frequency–size relation of earthquakes in a region can be approximated by the Gutenberg-Richter law ...
Earthquakes beneath our feet as well as stars iu the sky oeeur themore often, the less their magnitu...
Because earthquakes are the result of complex geophysical processes, it is not a simple matter to fi...
This paper is in continuation of previous investigations (Gutenbergand Richter, Paper I, 1942; Paper...
In a paper presented at a meeting of the Seismological Society of America on April 29, 1955, we have...
This supersedes Paper 1 (Gutenberg and Richter, 1942). Additional data are presented. Revisions invo...
Discrepancies arise among magnitudes as derived from local earthquake data (ML), body waves (MB) and...
This supersedes Paper 1 (Gutenberg and Richter, 1942). Additional data are presented. Revisions invo...
The magnitude of an earthquake was originally defined by the junior author (Richter, 1935), for sho...
Empirical relations involving seismic moment Mo, magnitude Ms, energy Es and fault dimension L (or...
Despite various shortcomings, the earthquake magnitude scale is one of the most fundamental earthqua...
Seismic magnitude is the quantitative measurement of amount of energy released by an earthquake. The...
Several studies have shown that local magnitude, M L, and moment magnitude, M , scale differently fo...
In the course of historical or statistical study of earthquakes in any given region it is frequentl...
The “revised magnitudes”, M, converted from Gutenberg's unified magnitude, m, and listed by Richter ...
Frequency–size relation of earthquakes in a region can be approximated by the Gutenberg-Richter law ...
Earthquakes beneath our feet as well as stars iu the sky oeeur themore often, the less their magnitu...
Because earthquakes are the result of complex geophysical processes, it is not a simple matter to fi...
This paper is in continuation of previous investigations (Gutenbergand Richter, Paper I, 1942; Paper...
In a paper presented at a meeting of the Seismological Society of America on April 29, 1955, we have...
This supersedes Paper 1 (Gutenberg and Richter, 1942). Additional data are presented. Revisions invo...
Discrepancies arise among magnitudes as derived from local earthquake data (ML), body waves (MB) and...
This supersedes Paper 1 (Gutenberg and Richter, 1942). Additional data are presented. Revisions invo...
The magnitude of an earthquake was originally defined by the junior author (Richter, 1935), for sho...
Empirical relations involving seismic moment Mo, magnitude Ms, energy Es and fault dimension L (or...
Despite various shortcomings, the earthquake magnitude scale is one of the most fundamental earthqua...
Seismic magnitude is the quantitative measurement of amount of energy released by an earthquake. The...
Several studies have shown that local magnitude, M L, and moment magnitude, M , scale differently fo...
In the course of historical or statistical study of earthquakes in any given region it is frequentl...
The “revised magnitudes”, M, converted from Gutenberg's unified magnitude, m, and listed by Richter ...
Frequency–size relation of earthquakes in a region can be approximated by the Gutenberg-Richter law ...
Earthquakes beneath our feet as well as stars iu the sky oeeur themore often, the less their magnitu...
Because earthquakes are the result of complex geophysical processes, it is not a simple matter to fi...