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《Chinese Journal of Geophysics》 1987-01
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A STUDY ON FINE STRUCTURE IN THE UPPER CRUST OF DUKOU AND ITS ADJACENT REGIONS

YIN ZHOU-XUN TENG JI-WEN XIONG SHAO-BAI(Institute of Geophysics, Acadcmia Sinica, Beijing)  
In order to study the deep crustal stru9ture in the Pan-Xi tectonic belt, a explosion seismic spunding along a profile of 350 km long in the Dukou region was conducted in 1984. The east-west profile from Zhehai to Lijiang was arranged and six seismic sections in the profile were obtained. In this paper, first seismic phases in records are analysed to study the upper crustal structure beneath Dukou in detail. In data processing we used different methods, such as theo-rerical travel time and ray tracing, for a model with lateral inhomogeneity and vertical gradient of velocity to fit the observed travel time data. Fine structures of the upper crust and velocity distributions down to 10 km deep are obtained.In 'the upper crust there exist several deep faults, which extend to the lower crust. The P wave velocity of 6.00 km/s between Dukou and Huaping is higher than those at the two ends of the profile (5.20 km/s in Zhehai and 3.5 km/s in Lijiang). The lateral variation of velocity seems to be attributed to tectonic processes. It is noted that there is a geological body with high velocity in the region between Dukou and Huaping, which is probably related to the upward .movement and concentration of magma from the upper mentle. It can be inferred that a great deal of mineral of sefstromite deposited in the Panzihua zone have somewhat relation with the above gebdynamic processes.
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