| 云南三江地区富碱侵入岩与煌斑岩的同源性 |
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| 引用本文： | 金志升,黄智龙,朱成明.云南三江地区富碱侵入岩与煌斑岩的同源性[J].矿物岩石地球化学通报,1997(4). |
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| 作者姓名： | 金志升 黄智龙 朱成明 |
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| 作者单位： | 中国科学院地球化学研究所 |
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| 摘 要： | 云南三江地区富碱侵入岩与煌斑岩的同源性金志升黄智龙朱成明（中国科学院地球化学研究所，贵阳５５０００２）关键词三江地区富碱侵入岩煌斑岩同源性三江地区富碱侵入岩带（亦称哀牢山－金沙江富碱侵入岩带）是世界上著名的富碱侵入岩带之一，前人对该区富碱侵入岩进行过...
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| 关 键 词： | 三江地区 富碱侵入岩 煌斑岩 同源性 |
Consanguinity of Alkaline Intrusions and Lamprophyres of Sanjiang District,Yunnan Province |
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| Jin Zhisheng,Huang Zhilong,Zhu Chengming.Consanguinity of Alkaline Intrusions and Lamprophyres of Sanjiang District,Yunnan Province[J].Bulletin of Mineralogy Petrology and Geochemistry,1997(4). |
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| Authors: | Jin Zhisheng Huang Zhilong Zhu Chengming |
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| Abstract: | The spatial distribution,yielding ages and trace elements,REE and isotope geochemistry data have been compared between alkaline intrusions and lamprophyres of Sanjiang alkaline intrusion zone in this paper.It is suggested that they are the products of comagmatic activity in the extension of mantle . The difference of trace elements and REE features between them maybe represent the different tendency and degree of magmatic evolution. |
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| Keywords: | Sanjiang district alkaline intrusion lamprophyres consanguinity |
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