| S is proportional to |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
| l | the total
linear size of earthquake sources |
||||||||||||
| if b=B/3 |
|||||||||||||
| l | the total
area of the earthquake sources |
||||||||||||
| if
b=2B/3 |
|||||||||||||
| l | the total
energy of earthquakes |
||||||||||||
| if b=B. |
|||||||||||||
| where B comes
from the relation between |
|||||||||||||
| the energy,
E, and magnitude, M |
|||||||||||||
| Iog
E = A + BM |
|||||||||||||
|
|
|
|
|
| Sixth
Workshop on Non-Linear |
||||
| Dynamics and Earthquake Prediction |
||||
| The Abdus Salam ICTP, Miramare |
||||
| 16/10/2001 |
| 11 |