Alfred Wegener, being a meteorologist, had proposed tidal forces and pole flight force as main driving mechanisms for continental drift. However, these forces were considered far too small to cause continental motion as the concept then was of continents plowing through oceanic crust.[20] Therefore, Wegener converted to convection currents as the main driving force in the last edition of his book in 1929.
In the plate tectonics context (accepted since the seafloor spreading proposals of Heezen, Hess, Dietz, Morley, Vine and Matthews (see below) during the early 1960s) though, oceanic crust is in motion with the continents which caused the proposals related to Earth rotation to be reconsidered. In more recent literature, these driving forces are:
- Tidal drag due to the gravitational force the Moon (and the Sun) exerts on the crust of the Earth[21]
- Shear strain of the Earth globe due to N-S compression related to the rotation and modulations of it;
- Pole flight force: equatorial drift due to rotation and centrifugal effects: tendency of the plates to move from the poles to the equator ("Polflucht");
- Coriolis effect acting on plates when they move around the globe;
- Global deformation of the geoid due to small displacements of rotational pole with respect to the Earth crust;
- Other smaller deformation effects of the crust due to wobbles and spin movements of the Earth rotation on a smaller time scale.
Of the many forces discussed in this paragraph, tidal force is still highly debated and defended as a possible principle driving force, whereas the other forces are used or in global geodynamic models not using the plate tectonics concepts (therefore beyond the discussions treated in this section), or proposed as minor modulations within the overall plate tectonics model.
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