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《Acta Geologica Gansu》 1984-00
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THE TECTONO-FORMATION ZONE AND CRUSTAL EVOLUTION OF DEVONIAN IN WESTERN QINLING RANGE

Zuo Guochao (Instiinte of Geology, Geological Bureau of Gansu)  
During Caledonian tectonic cycle the tectono-formation zone of Devoian in Western Qinling range is located at the triple junction of the Yangtze, the Songpan-Ganzi and North China plates.During Devonian plate motions had took place in this region. The fundamental tectono-formation zone was probably formed by diver-genting and convergenting of transform offset of moving Slabs.They may be divided into four zones: 1.Minxian-Lixian Shelf sea; 2.Diebu-Wudu mariginal arc of shelf sea; 3.Qiaotou-Kangxian trough; 4.Linjiang-Gaojiaba epicontinental sea.
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