GYIG OpenIR  > 矿床地球化学国家重点实验室
赣杭构造带东段661铀矿床成因机制探讨
田建吉; 胡瑞忠; 苏文超; 齐有强; 张国全; 商朋强
2015
Source Publication矿物学报
IssueS1Pages:346-347
Abstract

661铀矿床位于赣杭铀成矿带东段大洲铀矿田内,是我国最早发现的产在流纹岩中的铀矿床。由于前人对华南热液铀矿床的认识还存在种种争论及该矿床地球化学研究比较薄弱,以该矿床为研究对象,通过系统地球化学研究,结合区域成矿资料,探讨了该矿床可能的成矿作用机制。

Indexed ByCSCD
Language中文
Citation statistics
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/9650
Collection矿床地球化学国家重点实验室
Affiliation1.中核集团核工业北京地质研究院中核集团铀资源勘查与评价技术重点实验室
2.中国科学院地球化学研究所矿床地球化学国家重点实验室
3.浙江省有色金属地质勘查局
4.中化地质矿山总局地质研究院
Recommended Citation
GB/T 7714
田建吉,胡瑞忠,苏文超,等. 赣杭构造带东段661铀矿床成因机制探讨[J]. 矿物学报,2015(S1):346-347.
APA 田建吉,胡瑞忠,苏文超,齐有强,张国全,&商朋强.(2015).赣杭构造带东段661铀矿床成因机制探讨.矿物学报(S1),346-347.
MLA 田建吉,et al."赣杭构造带东段661铀矿床成因机制探讨".矿物学报 .S1(2015):346-347.
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