1987
DOI: 10.1016/0040-1951(87)90029-1
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Earthquake precursors in Japan: Precursor time and detectability

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Cited by 102 publications
(79 citation statements)
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“…On the basis of precursor data published up to 1977, Rikitake (1979) has given a relationship between precursor time (T) and earthquake magnitude (M) which was obtained on the basis of the best-fitting straight line using least square method as follows: log T = 0.6M − 1.01 . Rikitake (1987) modified the relation on the basis of 14 radon data sets and based on a general linear equation log T= a + bM, as: log T = (-0.47 ± 0.73) + (0.28 ± 0.12)M , which holds well for all the precursor disciplines. Using a log-linear relationship between precursor time and earthquake magnitude, Scholz et al (1973) established a relationship on the basis of a limited data set of radon anomalies as well as other precursors but this relationship was found to have a limited application (Hauksson, 1981).…”
Section: Empirical Algorithmsmentioning
confidence: 99%
“…On the basis of precursor data published up to 1977, Rikitake (1979) has given a relationship between precursor time (T) and earthquake magnitude (M) which was obtained on the basis of the best-fitting straight line using least square method as follows: log T = 0.6M − 1.01 . Rikitake (1987) modified the relation on the basis of 14 radon data sets and based on a general linear equation log T= a + bM, as: log T = (-0.47 ± 0.73) + (0.28 ± 0.12)M , which holds well for all the precursor disciplines. Using a log-linear relationship between precursor time and earthquake magnitude, Scholz et al (1973) established a relationship on the basis of a limited data set of radon anomalies as well as other precursors but this relationship was found to have a limited application (Hauksson, 1981).…”
Section: Empirical Algorithmsmentioning
confidence: 99%
“…It is known that the M-Dmax relation for geoscientific precursors can be approximately expressed by an equation similar to Eq. (1) (Rikitake, 1987). In obtaining Eq.…”
Section: Detectability As a Wholementioning
confidence: 99%
“…In order to see where a macro-anomaly precursor appears, the writer first of all examines the relation between earthquake magnitude (M) of the main shock and the epicentral distance (D) with respect to the data for the first six earthquakes in a fashion similar to the analysis for geoscientific precursors (Rikitake, 1987). Since the data are too numerous, the following approach is made to evaluate the overall tendency.…”
Section: Detectability As a Wholementioning
confidence: 99%
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