GIG OpenIR
梁培1,2; 陈华勇2; 赵联党3; Kendrick MARK4; 江宏君2,5; 张维峰6; 吴超2; 谢玉玲1
新疆北部弧-盆转化体系下铁氧化物-铜-金矿床的流体演化特征:来自卤族元素和稀有气体同位素的证据
Source Publication地学前缘
ISSN1005-2321
2020
Volume27Issue:3Pages:239-253
Language中文
EI Accession Number20202808932798
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/57096
Collection中国科学院广州地球化学研究所
Affiliation1.北京科技大学土木与资源工程学院,北京100083;
2.中国科学院广州地球化学研究所,广东广州510640;
3.长安大学地球科学与资源学院,陕西西安710064;
4.Research School of Earth Sciences,Australian National University,Acton 2601,Australia;
5.中国科学院大学,北京100049;
6.中国地质调查局武汉地质调查中心,湖北武汉430205
Recommended Citation
GB/T 7714
梁培,陈华勇,赵联党,等. 新疆北部弧-盆转化体系下铁氧化物-铜-金矿床的流体演化特征:来自卤族元素和稀有气体同位素的证据[J]. 地学前缘,2020,27(3):239-253.
APA 梁培.,陈华勇.,赵联党.,Kendrick MARK.,江宏君.,...&谢玉玲.(2020).新疆北部弧-盆转化体系下铁氧化物-铜-金矿床的流体演化特征:来自卤族元素和稀有气体同位素的证据.地学前缘,27(3),239-253.
MLA 梁培,et al."新疆北部弧-盆转化体系下铁氧化物-铜-金矿床的流体演化特征:来自卤族元素和稀有气体同位素的证据".地学前缘 27.3(2020):239-253.
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