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岩石学报  1989 

A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS
东秦岭与华南加里东褶皱带原地—准原地改造型花岗岩特征

Keywords: Source rocks,Granitoid Qinling,South China
源岩
,花岗岩,东秦岭,华南

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Abstract:

There is a great difference between the formation characteristics of South China and East Qinling Caledonian foldbelts. The difference makes the transformation type granitoids in the two foldbelts have different characteristics in chemical aspects. The characteristics of tranformation type granitoids are controlled by their source rocks to a great extent.

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