| 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 |
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| 引用本文： | 胡受奚,卢欣祥.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[J].岩石学报,1989,5(1):49-58. |
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| 作者姓名： | 胡受奚 卢欣祥 |
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| 作者单位： | 南京大学地球科学系，南京大学地球科学系，河南地质科学研究所 南京 210008，南京 210008，郑州 |
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| 摘 要： | 东秦岭与华南加里东褶皱带具有不同的岩石建造特征,两褶皱带的改造型花岗岩类之间也存在着明显不同的化学成分特征。研究表明源岩在很大程度上决定了改造型花岗岩的特征。
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| 关 键 词： | 源岩 花岗岩 东秦岭 华南 |
A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS |
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| Hu Shouxi Guo Jichuen.A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS[J].Acta Petrologica Sinica,1989,5(1):49-58. |
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| Authors: | Hu Shouxi Guo Jichuen |
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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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| Keywords: | Source rocks Granitoid Qinling South China |
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