| 浙江省明矾石矿床地质特征及其成因类型 |
| |
| 引用本文： | 吕惠进.浙江省明矾石矿床地质特征及其成因类型[J].化工矿产地质,2002,24(3):146-150. |
| |
| 作者姓名： | 吕惠进 |
| |
| 作者单位： | 浙江师范大学地理系 |
| |
| 基金项目： | 浙江省教育厅重点资助项目(980022) |
| |
| 摘 要： | 浙江非金属矿产资源丰富,其中明矾石等5种矿产的储量居全国首位,对明矾石资源的开发利用也居全国前列;但对其的控矿因素、成矿机理、成因类型的研究相对滞后。通过综合分析浙江省境内典型矿床的地质特征、成矿条件与环境,将其分成:火山喷发沉积-热液交代型、火山热液交代型两种类型。
|
| 关 键 词： | 明矾石 火山喷发沉积-热液交代 热液交代 浙江省 |
| 修稿时间： | 2002年6月10日 |
THE GEOLOGICAL CHARACTERISTICS AND TYPES OF CAUSE FOR FORMATION OF THE ALUNITE DEPOSITS IN ZHEJIANG PROVINCE |
| |
| Lu Huijin.THE GEOLOGICAL CHARACTERISTICS AND TYPES OF CAUSE FOR FORMATION OF THE ALUNITE DEPOSITS IN ZHEJIANG PROVINCE[J].Geology of Chemical Minerals,2002,24(3):146-150. |
| |
| Authors: | Lu Huijin |
| |
| Institution: | Geography Department ofZhejiang Normal University |
| |
| Abstract: | There are very abundant nonmetallic ore resources in Zhejiang province. The reserves of alunite and other five minerals are best abundant all over our country, and the exploiting and utilizing for alunite mineral resource is also in forefront. But the research in metallogenic factors, mechanism of mineralization and genetic types lags behind relatively. Based on the synthetical analyzing the geological characteristics, metallogenic conditions and their environment of model alunite deposits in Zhejiang province, they may be divided into two types: volcanic eruption volcanicerupion-sedimentary deposit and volcano hydrothermal-metasomatic deposit. |
| |
| Keywords: | Alunite volcanic eruption volcanicerupion-sedimentary deposit volcano hydrothermal-metasomatic deposit Zhejiang province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
