| 闾山花岗岩地质特征及其成因探讨 |
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| 引用本文： | 苏传玉,雷广新,刘文海,张兆华.闾山花岗岩地质特征及其成因探讨[J].国土资源,1994(Z1). |
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| 作者姓名： | 苏传玉 雷广新 刘文海 张兆华 |
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| 作者单位： | 辽宁省地质矿产局区域地质调查队 |
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| 摘 要： | 闾山花岗岩位于辽两台陷的东侧，是同源岩浆演化的多期产物。其物质源于地壳，一期结构演化规律强，是辽宁地区典型的“Ｓ”型花岗岩。
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| 关 键 词： | 闾山，超单元，稀土模式，“S’型花岗岩 |
GEOLOGICAL CHARACTERISTICS AND GENESIS OF GRANITE IN YIWULUSHAN |
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| Shu Chuanyu Lei Guangxin Liu Wenhai Zhang Zhaohua.GEOLOGICAL CHARACTERISTICS AND GENESIS OF GRANITE IN YIWULUSHAN[J].Land & Resources,1994(Z1). |
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| Authors: | Shu Chuanyu Lei Guangxin Liu Wenhai Zhang Zhaohua |
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| Abstract: | Tbe granite in Yiwulushan,located on the east sied West Liaoning syneclise,is theproduct of multiphase activities of comagma from the crust, which the first stage of textureevolution had a strong regular,so it belongs to a typical S-type granite. |
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| Keywords: | Yiwulushan ultra-unit REE model S-type granite |
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