作者: P. Brosche , J. Sündermann
DOI: 10.1007/978-94-010-1208-9_13
关键词: Solid earth 、 Tidal force 、 Geodesy 、 Period (geology) 、 Geology 、 Plate tectonics 、 Permian 、 Earth's rotation
摘要: Effects of the M2-tide have been calculated for a 4°-model present oceans and an approximate Pangea configuration continents at end Permian. From changes within tidal period, only movement solid Earth’ barycenter is order 2 cm. The net torque in accordance with astronomical value; smaller by factor 1/3 (the palaeontological evidence seems to indicate low values this later epochs). - question posed whether forces bottom friction may influence motions tectonic plates.