| 越城岭花岗岩主体的岩石学特征及其形成物理化学条件 |
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| 引用本文： | 姜德厚,陈克立,屠刚. 越城岭花岗岩主体的岩石学特征及其形成物理化学条件[J]. 桂林工学院学报, 1987, 0(Z1) |
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| 作者姓名： | 姜德厚 陈克立 屠刚 |
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| 作者单位： | 地质矿产勘查系(姜德厚，陈克立)，隐伏矿床预测研究所(屠刚) |
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| 摘 要： | 越城岭花岗岩主体属S型花岗岩。它是在3～7公里深处,相对还原和含水条件下,由岩浆结晶形成的。
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| 关 键 词： | 花岗岩 岩石学 岩石成因 |
PETROLOGICAL FEATURES AND PHYSICO-CHEMICAL COMDITIONS OF FORMATION OF THE MAIN BODY OF YUECHENGLING GRANITE |
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| Jiang Dehou,Chen Keli,Tu Gang. PETROLOGICAL FEATURES AND PHYSICO-CHEMICAL COMDITIONS OF FORMATION OF THE MAIN BODY OF YUECHENGLING GRANITE[J]. Journal of Guilin University of Technology, 1987, 0(Z1) |
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| Authors: | Jiang Dehou Chen Keli Tu Gang |
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| Affiliation: | Jiang Dehou;Chen Keli;Tu Gang Department of Exploration Geology Institute of Prediction of Hidden Ore Deposits |
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| Abstract: | The main body of Yuechengling granite is of S-type. The originalmagma crystallized at a depth of 3-7 km under relatiyely reducing andhydrous conditition. |
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| Keywords: | granite petrology lithogenesis |
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