| 浙东南地区次生石英岩型红柱石成矿地质特征及矿床成因初探 |
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| 引用本文： | 罗炎水,潘锦勃.浙东南地区次生石英岩型红柱石成矿地质特征及矿床成因初探[J].浙江国土资源,2001,17(1):45-51. |
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| 作者姓名： | 罗炎水 潘锦勃 |
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| 作者单位： | 浙江省第十一地质大队,温州,325006 |
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| 摘 要： | 浙东南地区次生石英岩型红柱石矿床为一种新的矿产类型,本文简要地总结该类矿床的地质特征和矿床特征,探讨了成矿地质条件和矿床成因,认为该类型红柱石矿床是由火山岩经火山热液蚀变形成次生石英岩,然后经热接触变质作用,致使部分铝硅酸盐矿物脱水分解形成红柱石矿床.
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| 关 键 词： | 红柱石 矿床地质特征 矿床成因 勘查开发 |
| 修稿时间： | 2000年8月15日 |
Discussions on One-Forming Geological Conditions and Genesis of Secondary Quartzite Andalusite Deposits in Southeastern Zhejiang |
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| Authors: | Luo Yanshui Pan Jinbo |
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| Abstract: | The secondary quartzite andalusite deposit in southeastern Zhejiang is a new type deposit.This paper mainly discusses mineralization conditions,deposit characteristics and genesis of this kind of deposits.It is thought that volcanic rocks firstly formed secondary quartzite by volcanie hydrothermal process,and then some aluminosilicate mincrals of their rocks formecl andalusite by contact thermal metamorphism. |
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| Keywords: | andalusite geological characteristics of the deposits genesis |
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