伟晶岩
地质学
地球化学
中国
锂(药物)
探矿
矿化(土壤科学)
沉积岩
构造学
锂同位素
古生物学
地理
土壤科学
化学
考古
离子交换
内分泌学
离子
土壤水分
有机化学
医学
作者
Jiankang Li,Tianren Zou,Xifang Liu,Denghong Wang,Ding Xin
标识
DOI:10.1111/1755-6724.12453
摘要
Abstract Lithium resources support the development of high‐technology industries. China has abundant lithium resources which are mainly distributed in Tibet, Qinghai, Sichuan and Jiangxi. Salt lakes in China have significant lithium reserves, but lithium is mainly produced from hard rock lithium deposits because the extraction from salt lakes requires further improvements. The hard rock lithium deposits mainly occur in granitic pegmatite in the Altay region of Xinjiang and the Jiajika deposit in western Sichuan Province; they mainly formed in the Mesozoic and occurred in a relatively stable stage during orogenic processes. On the basis of the information from 151 lithium deposits or spots, 14 lithium metallogenic series were identified, and granitic pegmatite, granite, and sedimentary types were considered to be the main prediction types of lithium resources. Twelve lithium mineralization belts were divided and a series of maps showing the lithium metallogenetic regularity in China were drawn. We conclude that the hard rock and brine type of lithium resources possibly have a similar lithium source related to magmatism. The metallogenic features of the lithium in China were related with the distinct history of tectonic‐magmatic activity in China. This study benefits the assessment of, and prospecting for, lithium resources in China.
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