Abstract
We demonstrate that the change of slope at t ⋍ − 0.1 ( GeV/c) 2 and the dip at t ⋍ − 1,4 ( GeV/c) 2 , observed in the recent ISR proton-proton elastic-scattering data, can both be simultaneously explained within the framework of Gribov's reggeon calculus for the pomeron.
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