过碱性岩
伟晶岩
蒸发岩
碳酸盐岩
地质学
地球化学
交代作用
锂辉石
地温梯度
经济短缺
锂(药物)
自然(考古学)
自然资源
自然资源经济学
矿物学
火山
古生物学
经济
材料科学
冶金
生态学
政府(语言学)
地幔(地质学)
哲学
陶瓷
沉积岩
内分泌学
语言学
生物
医学
作者
Robert Bowell,Laura Lagos,Camilo R. de los Hoyos,Julien Declercq
出处
期刊:Elements
[Mineralogical Society of America]
日期:2020-08-01
卷期号:16 (4): 259-264
被引量:115
标识
DOI:10.2138/gselements.16.4.259
摘要
There are three broad types of economic lithium deposit: 1) peralkaline and peraluminous pegmatite deposits and their associated metasomatic rocks; 2) Li-rich hectorite clays derived from volcanic deposits; 3) salar evaporites and geothermal deposits. Spodumene-bearing pegmatites are the most important and easily exploitable Li deposits, typically containing 0.5 Mt Li. Salar deposits hold the largest Li reserves, can reach up to 7 Mt Li, but are more difficult to exploit. Allowing for recycling, the current predicted demand up to the year 2100 is 20 Mt Li; world resources are currently estimated at more than 62 Mt Li. Thus, abundant resources exist, and no long-term shortage is predicted.
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