The scenario of a possible impact event of the Cretaceous-Paleogene boundary based on the "orbital" hypothesis

The studying the regions of global seismic belts, to which giant impact structures belong, confirms the hypothesis of the possible attachment to the Earth of its satellite at the Cretaceous-Paleogene boundary and the coincidence of these belts and structures to the routes of its tangent flight along the Med-Eocene position of the equator.