| 长乐-南澳构造带内的岩浆混合作用 |
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| 引用本文： | 聂童春.长乐-南澳构造带内的岩浆混合作用[J].福建地质,2007,26(4):270-279. |
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| 作者姓名： | 聂童春 |
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| 作者单位： | 福建省地质调查研究院,福州,350011 |
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| 基金项目： | 中国地质调查局,福建1∶25万周宁县(G50C001004)、福州市(G50C003004)、莆田市(G50C003004)、泉州市(G50C004004)幅区域地质调查)地调项目 |
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| 摘 要： | 长乐—南澳构造带由于其特殊的地质构造背景,形成诸多具有典型意义的地质构造现象,岩浆混合作用形成的各类地质现象是其中的一类,通过对大量野外资料的分析,将岩浆混合作用划分为3个不同阶段,并结合区域构造背景探讨了各个阶段岩浆混合作用发生的机制,对进一步研究该构造带提供了重要的信息。
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| 关 键 词： | 岩浆混合 酸性端元 基性端元 长乐—南澳 |
| 收稿时间： | 2007-07-28 |
| 修稿时间： | 2007年7月28日 |
Magmatic Mixing in the Changle-Nan'ao Tectonic Belt |
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| Nie Tongchun.Magmatic Mixing in the Changle-Nan''''ao Tectonic Belt[J].Geology of Fujian,2007,26(4):270-279. |
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| Authors: | Nie Tongchun |
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| Abstract: | There are many typical and significant geological structures in the Changle-Nan'ao tectonic belt which has many specific geological structures,one kind of which the deferent geologic structures formed by the magmatic mixing are.Based on the a great quantity of field geological data,it is considered that the magmatic mixing can be divided into three stages.In the paper,it makes a study of the mechanism of deferent magmatic mixing according to the background of regional geologic structures,which makes an offer of some important information for further research of the Changle-Nan'ao tectonic belt. |
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| Keywords: | magmatic mixing acidic end-member basic end-member Changle-Nan'ao tectonic belt |
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