The intranuclear cascade (INC) plus evaporation model for nucleon-nucl
eus interactions in the 200 MeV-1.2 GeV range is revisited. The standa
rd Liege INC model supplemented by the Dresner evaporation-fission mod
el is used and shown to give a good overall agreement with experimenta
l data, basically neutron double differential cross-sections and resid
ue mass spectra. Small systematic discrepancies are identified and sho
wn to correspond to the single scattering contribution. Improvements o
f the INC model, linked with in-medium cross-sections, refraction of p
articles at the nuclear surface, treatment of the Pauli blocking, desc
ription of nuclear surface, collision mode and hadronisation time are
discussed. The problem of the stopping time at which the cascade model
gives place to the evaporation model is examined in detail. The intro
duction of a pre-equilibrium step, intermediate between the cascade an
d evaporation steps is investigated and shown to bring no significant
improvement of the predictions. The production of composites and of in
termediate mass fragments is shortly studied, with the help of the sta
ndard model, of the three step model mentioned above and of a cascade
plus percolation model. (C) 1997 Elsevier Science B.V.