Possibility of Estimating the Maximum Earthquake Magnitude Based on a Modified G-R Model for Magnitude-Frequency Distribution
نویسندگان
چکیده
منابع مشابه
Fractal dimension and earthquake frequency-magnitude distribution in the North of Central-East Iran Blocks (NCEIB)
The Gutenberg–Richter parameters (a and b), fractal dimension (DC), and relationships between these parameters are calculated for different regions of the North of Central-East Iran Blocks (NCEIB). The whole examined area (between 34°-36° N and 55°-61° E) is divided into 55 equal square grids. Both the a and b values for the frequency-magnitude distribution (FMD) and the fractal dimension (DC) ...
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This paper provides a generic equation for the evaluation of the maximum earthquake magnitude mmax for a given seismogenic zone or entire region. The equation is capable of generating solutions in different forms, depending on the assumptions of the statistical distribution model and/or the available information regarding past seismicity. It includes the cases (i) when earthquake magnitudes are...
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ACKNOWLEDGEMENTS I would like to thank my primary advisor Dr. Andrew V. Newman for providing his excellent guidance and scientific insight throughout the study. I am thankful to Dr. for their thoughtful advice and suggestions. I am grateful to Dr. Tapas Bhattacharyya for the stimulating discussions and his support. I would also like to thank numerous prior and recent earthquake analysts, includ...
متن کاملfractal dimension and earthquake frequency-magnitude distribution in the north of central-east iran blocks (nceib)
the gutenberg–richter parameters (a and b), fractal dimension (dc), and relationships between these parameters are calculated for different regions of the north of central-east iran blocks (nceib). the whole examined area (between 34°-36° n and 55°-61° e) is divided into 55 equal square grids. both the a and b values for the frequency-magnitude distribution (fmd) and the fractal dimension (dc) ...
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Qualitative interaction (Peto, 1982) is a useful concept, but its practical value i~ limited because its presence is hard to detect. This difficulty arises from trying to detect a treatment effect of opposite direction to the main effect in a small number of subgroups. Simulation results are presented which reinforce this point. A new measure of interaction magnitude, I AI, is introduced and pr...
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ژورنال
عنوان ژورنال: Zisin (Journal of the Seismological Society of Japan. 2nd ser.)
سال: 2003
ISSN: 0037-1114,1883-9029,2186-599X
DOI: 10.4294/zisin1948.56.3_255