GIG OpenIR  > 同位素地球化学国家重点实验室
王雅美1,2; 尹继元2; 袁超3; 肖文交4,5; 陈文2; 蔡克大1; 杨雪叶1,2; 陶再礼1,2
新疆西准噶尔苏云河斑岩型钼矿的剥露和保存条件:来自裂变径迹和(U-Th)/He热年代学的约束
Source Publication岩石学报
ISSN1000-0569
2021
Volume37Issue:8Pages:2547-2561
Language中文
CSCD IDCSCD:7050884
Indexed BySCI ; EI ; CSCD
Citation statistics
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/63640
Collection同位素地球化学国家重点实验室
Affiliation1.中国地质大学(北京)地球科学与资源学院,北京100083;
2.中国地质科学院地质研究所,自然资源部深地动力学重点实验室,北京100037;
3.中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广州510640;
4.中国科学院新疆生态与地理研究所新疆矿产资源研究中心,乌鲁木齐830011;
5.中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室,北京100029
Recommended Citation
GB/T 7714
王雅美,尹继元,袁超,等. 新疆西准噶尔苏云河斑岩型钼矿的剥露和保存条件:来自裂变径迹和(U-Th)/He热年代学的约束[J]. 岩石学报,2021,37(8):2547-2561.
APA 王雅美.,尹继元.,袁超.,肖文交.,陈文.,...&陶再礼.(2021).新疆西准噶尔苏云河斑岩型钼矿的剥露和保存条件:来自裂变径迹和(U-Th)/He热年代学的约束.岩石学报,37(8),2547-2561.
MLA 王雅美,et al."新疆西准噶尔苏云河斑岩型钼矿的剥露和保存条件:来自裂变径迹和(U-Th)/He热年代学的约束".岩石学报 37.8(2021):2547-2561.
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