Abstract:We found that there were a series of granitoid and volcanic rock,which did not relate to the environment of active continental margin when we study the southern Chinese Altay orogenic belt.They formed...We found that there were a series of granitoid and volcanic rock,which did not relate to the environment of active continental margin when we study the southern Chinese Altay orogenic belt.They formed in the environment of psssive continental margin and related to extension of continental crust. We call the continental margin Passive Continental Margin with Magmatism in order to differentiate from amagmatic passive continental marginRead More
Publication Year: 1996
Publication Date: 1996-01-01
Language: en
Type: article
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