Geophysical basis for crustal deformation under the Tibetan Plateau

Details Geophysical basis for crustal deformation under the Tibetan Plateau Geophysical basis for crustal deformation under the Tibetan Plateau

Dec 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985pepi...41..170h&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 41, Issue 2-3, p. 170-185.

Physics

5

Scientific paper

This paper uses plate tectonics and satellite-derived gravity data to further discussion of crustal deformation under the Tibetan Plateau. The first of our three contributions is a spherical harmonic analysis of the global plate boundary system. A distribution of 470 Dirac delta functions is applied to describe the generating forces according to the rates of crustal creation and destruction on the plate boundaries. Analysis of the extensional and compressional forces in the spreading and subducting zones shows that the present global plate motion causes compressional stresses in the N-S direction under the Tibetan Plateau. The second contribution is the calculation of the crustal stresses in Tibet as inferred from satellite gravity data. By applying solutions to the problem of the spherical shells, the satellite-determined stresses indicate that the upwelling mantle material under Tibet induce N-S and E-W extension. Finally, a superimposed stress system is constructed. This stress system shows that the present crustal deformation in Tibet does not produce N-S shortening but generates E-W extension.
The results of this paper have provided geophysical explanations for geological field observations in Tibet and fault plane solutions of earthquakes in the Tibetan side of the India-Eurasia collison. The stress patterns reveal that the cold downwelling mantle convection flow beneath southern Tibet pulls the Indian plate down but applies a bending moment on the end of the plate to uplift and support the mass of the Himalayas.

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