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《Chinese Journal of Sinica》 1973-01
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GRAVITY COMPENSATION OF THE MOHOROVICIC DISCONTINUITY AND THE BASIC MODEL OF CRUSTAL STRUCTURE

TSENG JUNG-SHENG  
In this paper,the relationship between the average thickness of the earth crust obtained from Rayleigh-wave dispersion and the surface topography is discussed.In East China,this relationship can be expressed by two different straight lines.It is concluded that the crust in this area may be divided into two separate regions,the North and the South,each of which is an indepedent isostatic system at the depth of Mohorovicic discontinuity.The earth crust in western China belongs to other different isostatie systems.There is evident correlation between this crustal regionalization and geological phenomena.
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