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THE INVERSION OF THE CRUSTAL STRUCTURES FROM THE TRAVEL TIMES OF BODY WAVES

DING YUN-TU(The Seismolagical Bureau of Shanxi Province)  
The fundamental principles of deducing parameters of a homogeneous, horizontally layered crustal model from the inversion of the travel times of body waves are developed and two effective inversion methods are presented: the '' layered inversion'' under some restraints and the '' composite in version'' of several seismic phases. Some artificial models are tested and a satisfactory solution may be obtained by either of the two methods.
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