| 别珍套(山)花岗岩带地质特征及含矿性 |
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| 引用本文： | 董占清,田阔邦,张兴龙.别珍套(山)花岗岩带地质特征及含矿性[J].新疆地质,1989(2). |
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| 作者姓名： | 董占清 田阔邦 张兴龙 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第一区调大队
(董占清，田阔邦)，新疆维吾尔自治区地质矿产局第一区调大队(张兴龙) |
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| 摘 要： | 别珍套花岗岩带花岗岩为S型花岗岩.各岩体分异充分.为岩浆晚期产物.对稀有稀土元素成矿有利.
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| 关 键 词： | S型花岗岩 岩浆晚期 稀有稀土元素成矿 |
GEOLOGIC CHARACTERISTICS AND MINERALIZATION OF BEGJINTAW GRANITE BELT, XINJIANG |
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| Dong Zhanqing Tian Kuobang Zhang Xinglong.GEOLOGIC CHARACTERISTICS AND MINERALIZATION OF BEGJINTAW GRANITE BELT, XINJIANG[J].Xinjiang Geology,1989(2). |
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| Authors: | Dong Zhanqing Tian Kuobang Zhang Xinglong |
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| Abstract: | The granite of Begjintaw granite belt is of S-granite type. The granite bodies are well segregeted, which are the products of late stage of magmatism. They are in favour of the mineralization of rare elements and rare earth elements. |
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| Keywords: | S-granlte type late magmatic stoping metallogenesis of rare element and REE |
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