Earthquake duration magnitude
id:
earthquake-duration-magnitude-258-13843848
title:
Earthquake duration magnitude
text:
The concept of Earthquake Duration Magnitude – originally proposed by E. Bisztricsany in 1958 using surface waves only - is based on the realization that on a recorded earthquake seismogram, the total length of the seismic wavetrain – sometimes referred to as the CODA – reflects its size. Thus larger earthquakes give longer seismograms [as well as stronger seismic waves] than small ones. The seismic wave interval measured on the time axis of an earthquake record - starting with the first seismic
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wiki
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encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Earthquake_duration_magnitude
date created:
date modified:
2022-10-22T11:38:25Z
main entity:
{"identifier":"Q5327267","url":"https://www.wikidata.org/entity/Q5327267"}
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13
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13