Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9157
AuthorsScalera, G. 
TitleCoriolis effect as cause of East-West Earth's asymmetry
Issue DateNov-2014
URIhttp://hdl.handle.net/2122/9157
KeywordsCoriolis effect in deep Earth
Earth's expansion
Extrusion of deep mantle materials
Emitting Earth
Subject Classification04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes 
04. Solid Earth::04.01. Earth Interior::04.01.03. Mantle and Core dynamics 
04. Solid Earth::04.03. Geodesy::04.03.02. Earth rotation 
04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics 
AbstractThe different slope of the Wadati-Benioff zones oriented towards east and west is considered a main asymmetry of the Earth's globe. Under the Americas they have angles of about 30o, while under the Pacific east coasts (Asia, Japan) the angles are steeper. In the framework of plate tectonics geodynamics the cause of this difference can be identified in the tidal drag that would cause a global shift of the lithosphere towards west. But this solution has been many times criticized on the basis of the irrelevance of the tidal forces with respect to viscous friction. Instead, it is possible to show that in a different framework, in which sudden extrusions of mantle materials occur by local phase change toward a more unpacked lattice, the value of the Coriolis fictitious force can rise of several magnitude orders, becoming the main cause of the east-west asymmetry of the Wadati-Benioff zones, which might be ascribed entirely to internal causes of the planet (its rotation and geodynamics) and not to external causes (influence of other celestial bodies). Some astrogeodetic clues supporting the new geodynamic scenario are scrutinized.
DescriptionRevealing a serius omission of the 'main stream'
Appears in Collections:Manuscripts

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