The formation of the giant Huayangchuan U-Nb deposit associated with carbonatite in the Qingling Orogenic Belt | |
Xue, Shuo2,9; Ling, Ming-Xing8; Liu, Yu-Long7; Kang, Qing-Qing6; Huang, Rui-Fang5; Zhang, Zhe-Kun2,9; Sun, Weidong1,2,3,4 | |
刊名 | ORE GEOLOGY REVIEWS |
2020-07-01 | |
卷号 | 122页码:16 |
ISSN号 | 0169-1368 |
DOI | 10.1016/j.oregeorev.2020.103498 |
WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
语种 | 英语 |
WOS记录号 | WOS:000537805900047 |
内容类型 | 期刊论文 |
源URL | [http://ir.gig.ac.cn/handle/344008/57607] |
专题 | 同位素地球化学国家重点实验室 中国科学院矿物学与成矿学重点实验室 |
通讯作者 | Ling, Ming-Xing |
作者单位 | 1.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanog, Qingdao 266071, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 5.Southern Univ Sci & Technol, SUSTech Acad Adv Interdisciplinary Studies, Shenzhen 518055, Peoples R China 6.Team 224 Sino Shaanxi Nucl Ind Grp, Xian 710100, Peoples R China 7.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China 8.East China Univ Technol, State Key Lab Nucl Resources & Environm, Nanchang 330013, Jiangxi, Peoples R China 9.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China |
推荐引用方式 GB/T 7714 | Xue, Shuo,Ling, Ming-Xing,Liu, Yu-Long,et al. The formation of the giant Huayangchuan U-Nb deposit associated with carbonatite in the Qingling Orogenic Belt[J]. ORE GEOLOGY REVIEWS,2020,122:16. |
APA | Xue, Shuo.,Ling, Ming-Xing.,Liu, Yu-Long.,Kang, Qing-Qing.,Huang, Rui-Fang.,...&Sun, Weidong.(2020).The formation of the giant Huayangchuan U-Nb deposit associated with carbonatite in the Qingling Orogenic Belt.ORE GEOLOGY REVIEWS,122,16. |
MLA | Xue, Shuo,et al."The formation of the giant Huayangchuan U-Nb deposit associated with carbonatite in the Qingling Orogenic Belt".ORE GEOLOGY REVIEWS 122(2020):16. |
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