Basins for general nonlinear hénon attracting sets

When a new homoclinic intersection is created for a dissipative diffeomorphism in dimension two, there results a cascade of sinks. We show that immediately after one of these sinks q_n is formed, its basin boundary is made up of the stable manifold of the saddle periodic point p_n formed at the same time. After this sink undergoes a period doubling, there still remains a trapping region with an attracting set inside. In fact, we show that until this saddle periodic point pn has its own homoclinic bifurcation, there is an attracting set whose boundary is made up of the stable manifold of pn- By picking a rectangle B_n carefully, the one-parameter family of maps f_tn creates these sinks and attracting sets by pulling the image f_tn(B_n) across B_n and eventually forming a horseshoe in B_n. The maps, f_tn on B_n, are well approximated for large n by quadratic maps equivalent to the Hénon map. We prove our results for general nonlinear Hénon maps which include not only the quadratic maps but also other nonlinear maps which also create horseshoes, including those arising from homoclinic tangencies.