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THE EVOLUTION OF PALEOPLATES IN THE KANG-DIAN TECTONIC ZONE

Luo Yiaonan (Panxi Geological Team of Sichuan Province)  
A scries of important geological cvcntsin the kang-Dian tectonic zone has been reexamined from the plate tectonics point of view. It is suggested that this zone was an ancient island-are, similar to the present are-trench system along the W. Pacific, with the central Szechuan miccontinent to its east and an oceanic plate to its west. During the Jinning movement, it was folded and transformed into an active continental margin of the Appalachian type, which was then turned into a postorogenic rifts of the type of the basin-range province in the W. U. S. A.. From the late Sinian to early paleozoic there was a development of the stable intraplate-platform. Another continental rifting in the tectonic zone came in the late Paleozoic and ended up in Eocene, with much likeness to the East African rift systems of the arch volcano type. On the basis of the historic records of petrography of plate tectonics, analysis of typical sedimentation facits and formations in their successions, tecto no-thermal events as well as radio chronolegical data, emphasis is put on the tectonic evolution of the plates in three stages since the mid Proterozoic , i. e. , formation of the zone as anisland are fold belt, the Caledonian prerif-ting antcclise rise and the development and failure of the Hercyno Hymalay-an continental rift zone.
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