Of overlapping Cantor sets and earthquakes: Analysis of the Chakrabarti-Stinchcombe model
نویسنده
چکیده
We report an exact analysis of a discrete form of the ChakrabartiStinchcombe model for earthquakes [Physica A 270, 27 (1999)] which considers a pair of dynamically overlapping finite generations of the Cantor set as a prototype of geological faults. In this model the n-th generation of the Cantor set shifts on its replica in discrete steps of the length of a line segment in that generation and periodic boundary conditions are assumed. We determine the general form of time sequences for the constant magnitude overlaps and hence obtain the complete time-series of overlaps by the superposition of these sequences for all overlap magnitudes. From the time-series we derive the exact frequency distribution of the overlap magnitudes. The corresponding probability distribution of the logarithm of overlap magnitudes for the n-th generation is found to assume the form of the binomial distribution for n Bernoulli trials with probability 1/3 for the success of each trial. For an arbitrary pair of consecutive overlaps in the time-series where the magnitude of the earlier overlap is known, we find that the magnitude of the later overlap can be determined with a definite probability; the conditional probability for each possible magnitude of the later overlap follows the binomial distribution for k Bernoulli trials with probability 1/2 for the success of each trial and the number k is determined by the magnitude of the earlier overlap. Though this model does not produce the Gutenberg-Richter law for earthquakes, our results indicate that the fractal structure of faults admits a probabilistic prediction of earthquake magnitudes. PACS numbers: 05.45.Tp, 05.45.Df, 91.30.Px ∗[email protected]
منابع مشابه
Of overlapping Cantor sets and earthquakes: Analysis of the discrete Chakrabarti-Stinchcombe model
We report an exact analysis of a discrete form of the ChakrabartiStinchcombe model for earthquakes [Physica A 270, 27 (1999)] which considers a pair of dynamically overlapping finite generations of the Cantor set as a prototype of geological faults. In this model the n-th generation of the Cantor set shifts on its replica in discrete steps of the length of a line segment in that generation and ...
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تاریخ انتشار 2008