Metallogenic mechanism and prospect of key metal beryllium
文献类型：期刊论文
| 作者 | Rao Can1; Wang RuCheng2; Che XuDong2; Li XiaoFeng3; Wang Qi1; Zhang ZhiQi1; Wu RunQiu1 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2022-07-01 |
| 卷号 | 38期号:7页码:1848-1860 |
| 关键词 | Key metal beryllium Be-bearing minerals Be resources Deposit types of Be Metallogenic potential |
| ISSN号 | 1000-0569 |
| DOI | 10.18654/1000-0569/2022.07.02 |
| 英文摘要 | Beryllium ( Be) is one of the unsubstitutable key metals in strategic emerging industries and national defense industries, where its occurrence, metallogenic mechanisim and resource distribution are most important contents in the research of key metal minerals. Beryllium is one of incompatible elements, which can't enter into most rock -forming minerals, and tends to be enriched and crystallized during the late magmatic stages or even hydrothermal stages. However, beryllium is a typical amphoteric element, and can be enriched and precipitated in both acidic and alkaline environments. Most granitic rocks, alkaline rocks and their related rocks are thus the main carriers of beryllium ore. Be deposits related to magmatic-hydrothermal process mainly include "volcanogenic type" Be ore, highly differentiated granite -pegmatite type Be ore, greisen quartzite type Be ore, alkaline rock type Be ore, skarn type Be ore, and carbonatite type Be ore, and so on. The concentration, migration, crystallization and mineralization of beryllium are absolutely controlled by the differentiation of acidic and alkaline magma, magmatic-hydrothermal processes and volatile component content. Together with other rare earth metal elements, moreover, beryllium is often mineralized to form symbiotic deposits and associated deposits. In the exploitation processes, we should pay attention to improve the metallurgical processes such as separation process and purification process. It is expected to make a breakthrough in granite type, pegmatite type and "volcanogenic type" Be ores in our country. The southeast coastal volcanic rock area, Greater Khingan volcanic rock area, southern Tibet and central -western Xinjiang can become important target areas of Be resources. |
| WOS关键词 | TOPAZ-LEPIDOLITE GRANITE ; TRACE-ELEMENTS ; GEOCHEMICAL EVOLUTION ; FLUID INCLUSIONS ; SPOR MOUNTAIN ; MINERALIZATION ; PEGMATITE ; DEPOSIT ; PROVINCE ; RARE |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000878167100001 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/107711]  |
| 专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
| 通讯作者 | Rao Can |
| 作者单位 | 1.Zhejiang Univ, Sch Earth Sci, Key Lab Geosci Big Data & Deep Resource Zhejiang, Hangzhou 310027, Peoples R China 2.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Rao Can,Wang RuCheng,Che XuDong,et al. Metallogenic mechanism and prospect of key metal beryllium[J]. ACTA PETROLOGICA SINICA,2022,38(7):1848-1860. |
| APA | Rao Can.,Wang RuCheng.,Che XuDong.,Li XiaoFeng.,Wang Qi.,...&Wu RunQiu.(2022).Metallogenic mechanism and prospect of key metal beryllium.ACTA PETROLOGICA SINICA,38(7),1848-1860. |
| MLA | Rao Can,et al."Metallogenic mechanism and prospect of key metal beryllium".ACTA PETROLOGICA SINICA 38.7(2022):1848-1860. |
入库方式： OAI收割
来源：地质与地球物理研究所
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