The cr-zr-ca armalcolite in lunar rocks is loveringite: Constraints from electron backscatter diffraction measurements | |
Ai-Cheng Zhang; Run-Lian Pang; Naoya Sakamoto; Hisayoshi Yurimoto | |
2020 | |
Source Publication | American Mineralogist
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Volume | 105Issue:7Pages:1021-1029 |
DOI | 10.2138/am-2020-7260 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/11681 |
Collection | 矿床地球化学国家重点实验室 |
Affiliation | 1.State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China 2.Isotope Imaging Laboratory, Creative Research Institution, Hokkaido University, Sapporo 001-0021, Japan 3.Department of Natural History Sciences, Hokkaido University, Sapporo 060-0810, Japan 4.Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, Kanagawa 252-5210, Japan 5.CAS Center for Excellence in Comparative Planetology, China |
Recommended Citation GB/T 7714 | Ai-Cheng Zhang,Run-Lian Pang,Naoya Sakamoto,et al. The cr-zr-ca armalcolite in lunar rocks is loveringite: Constraints from electron backscatter diffraction measurements[J]. American Mineralogist,2020,105(7):1021-1029. |
APA | Ai-Cheng Zhang,Run-Lian Pang,Naoya Sakamoto,&Hisayoshi Yurimoto.(2020).The cr-zr-ca armalcolite in lunar rocks is loveringite: Constraints from electron backscatter diffraction measurements.American Mineralogist,105(7),1021-1029. |
MLA | Ai-Cheng Zhang,et al."The cr-zr-ca armalcolite in lunar rocks is loveringite: Constraints from electron backscatter diffraction measurements".American Mineralogist 105.7(2020):1021-1029. |
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