Theory of multicolor lattice gas: a cellular automaton Poisson solver
Journal of Computational Physics
Models of earthquake faults with long-range stress transfer
Computing in Science and Engineering
A TCAD system for VLSI implementation of the CVD process using VHDL
Integration, the VLSI Journal
Theory of Self-Reproducing Automata
Theory of Self-Reproducing Automata
Environmental Modelling & Software
iCity: A GIS-CA modelling tool for urban planning and decision making
Environmental Modelling & Software
Modeling of the 2001 lava flow at Etna volcano by a Cellular Automata approach
Environmental Modelling & Software
A macroscopic collisional model for debris-flows simulation
Environmental Modelling & Software
A tool to improve the execution time of air quality models
Environmental Modelling & Software
Artificial Intelligence techniques: An introduction to their use for modelling environmental systems
Mathematics and Computers in Simulation
MCA model for simulating the failure of microinhomogeneous materials
Journal of Nanomaterials
Microprocessors & Microsystems
Advances in Engineering Software
CAOS: a domain-specific language for the parallel simulation of cellular automata
PaCT'07 Proceedings of the 9th international conference on Parallel Computing Technologies
Cellular automata on FPGA for real-time urban traffic signals control
The Journal of Supercomputing
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Seismicity is an extended geophysical characteristic of the Greek dominion. There are certain areas of high seismic activity, as well as, regions of low seismicity where strong earthquakes are rather rare events. Consequently, it is of great interest to present a methodology concerning the earthquake process in Greece even for areas considered to be of low seismicity. In this paper, a study of the earthquake activity of an area in Northeastern Greece, centred at Xanthi, Thrace, extending over a region of radius R=80km, during a certain time period is presented. A two-dimensional cellular automaton (CA) dynamic system consisting of cells representing charges is used for the simulation of the earthquake process. The model has been tested as well as calibrated using the recorded events of the above-mentioned region as initial conditions. The simulation results are found in good quantitative and qualitative agreement with the Gutenberg-Richter (GR) scaling relations. Finally, the CA model has a user-friendly interface and enables the user to change several of its parameters, in order to study various hypotheses concerning the seismicity of the region under consideration.