ABSTRACT: A statistical method of detecting dependent events and aftershocks using spatial and temporal information was develop-ed and applied to Japan and California earthquake catalogs. On the basis of a statistic s s = 7r 2kt where r is the distance between two events, k is the normal earthquake rate and t is the time interval between the events, a decision was made whether a pair of events were dependent. The theoretical distribution of s for a catalog consisting of only independent events was compared to the actual catalogs. On the basis of the differences between the distributions, the number of inferred dependent events was determined. This discrimination technique was applied to the earth-quake catalogs of Northern Japan (1926-1960)...
Statistical studies on earthquake recurrence time probabilities have frequently been applied to seis...
The most used and accepted models for daily forecasts are based on short-term space and time earthqu...
The concept of background seismicity is strictly related to the identification of spontaneous and tr...
We investigated the foreshock activity characteristics using the Japan Meteorological Agency Unified...
International audienceA method for measuring seismicity rate changes caused by the occurrence of maj...
A standard approach to quantifying the seismic hazard is the relative intensity (RI) method. It is a...
In the context of seismic hazard quantification, the main objective of statistically analyzing an ea...
Applying a simple general procedure for identifying aftershocks, we inves- tigate their statistical ...
We propose a fast method able to discriminate between Poissonian independent earthquakes and aftersh...
This study provides systematic analysis of points of structural change in probability distributions....
The seismic generation rate, SGR, at southern California along the 1981–2007 recording period is ana...
In this paper, waveform similarity analysis is adapted and implemented in a declustering procedure t...
[1] We use recent results on statistical analysis of seismicity to present a robust method for compr...
Based on the ETAS (epidemic-type aftershock sequence) model, which is used for describing the featur...
The main goal of this thesis is to analyze the statistical properties of seismic catalogues of natur...
Statistical studies on earthquake recurrence time probabilities have frequently been applied to seis...
The most used and accepted models for daily forecasts are based on short-term space and time earthqu...
The concept of background seismicity is strictly related to the identification of spontaneous and tr...
We investigated the foreshock activity characteristics using the Japan Meteorological Agency Unified...
International audienceA method for measuring seismicity rate changes caused by the occurrence of maj...
A standard approach to quantifying the seismic hazard is the relative intensity (RI) method. It is a...
In the context of seismic hazard quantification, the main objective of statistically analyzing an ea...
Applying a simple general procedure for identifying aftershocks, we inves- tigate their statistical ...
We propose a fast method able to discriminate between Poissonian independent earthquakes and aftersh...
This study provides systematic analysis of points of structural change in probability distributions....
The seismic generation rate, SGR, at southern California along the 1981–2007 recording period is ana...
In this paper, waveform similarity analysis is adapted and implemented in a declustering procedure t...
[1] We use recent results on statistical analysis of seismicity to present a robust method for compr...
Based on the ETAS (epidemic-type aftershock sequence) model, which is used for describing the featur...
The main goal of this thesis is to analyze the statistical properties of seismic catalogues of natur...
Statistical studies on earthquake recurrence time probabilities have frequently been applied to seis...
The most used and accepted models for daily forecasts are based on short-term space and time earthqu...
The concept of background seismicity is strictly related to the identification of spontaneous and tr...