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heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple

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Page 1: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 2: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 3: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 4: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 5: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 6: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 7: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 8: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 9: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 10: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 11: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 12: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 13: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 14: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 15: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 16: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple
Page 17: heatont/papers/Microscopic and...Q/CpSw= ŒfD/Cpw (1) where C is the specific heat, and p is the density. In general D increases with the earthquake magnitude, MY. Here we use a simple

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