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  • 1
    Electronic Resource
    Electronic Resource
    Oceanic subcrustal flow toward the continents and constancy of global sea-level (1969)
    Springer
    Pure and applied geophysics 72 (1969), S. 117-122 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00875698
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