Metallogenic mechanism and prospect of key metal beryllium

doi:10.18654/1000-0569/2022.07.02

	Metallogenic mechanism and prospect of key metal beryllium
	Rao Can 1; Wang RuCheng 2; Che XuDong 2; Li XiaoFeng 3; Wang Qi 1; Zhang ZhiQi 1; Wu RunQiu 1
	2022-07-01
Source Publication	ACTA PETROLOGICA SINICA
ISSN	1000-0569
Volume	38 Issue:7 Pages:1848-1860
Abstract	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.
Keyword	Key metal beryllium Be-bearing minerals Be resources Deposit types of Be Metallogenic potential
DOI	10.18654/1000-0569/2022.07.02
WOS Keyword	TOPAZ-LEPIDOLITE GRANITE ; TRACE-ELEMENTS ; GEOCHEMICAL EVOLUTION ; FLUID INCLUSIONS ; SPOR MOUNTAIN ; MINERALIZATION ; PEGMATITE ; DEPOSIT ; PROVINCE ; RARE
Language	英语
WOS Research Area	Geology
WOS Subject	Geology
WOS ID	WOS:000878167100001
Publisher	SCIENCE PRESS
Citation statistics
Document Type	期刊论文
Identifier	http://ir.iggcas.ac.cn/handle/132A11/107711
Collection	矿产资源研究院重点实验室
Corresponding Author	Rao Can
Affiliation	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
Recommended Citation 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.

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