Rise of activity, i.e. inverse cascading, at the approach of an extreme event

Data


l	Catalog of main shocks:

{t_i, m_i, h_i, b_i(e)}, i = 1, 2 ...

Here t_i is the origin time, t_i£ t_i+1; m_i is
	the magnitude, h_i is focal depth,
	and b_i(e) is the number of
	aftershocks with magnitude M_aft or
	more during the first e days.


		Sixth Workshop on Non-Linear
Dynamics and Earthquake Prediction
	The Abdus Salam ICTP, Miramare

22/10/2001