文献
J-GLOBAL ID:202002212606698411
整理番号:20A2148252
東太平洋海膨(2.6~3.1°S)における不均質マントル融解とマグマ過程:中央海嶺玄武岩地球化学とSr-Nd-Pb同位体からの証拠【JST・京大機械翻訳】
Heterogeneous mantle melting and magmatic processes at the East Pacific Rise (2.6-3.1°S): Evidence from mid-ocean ridge basalt geochemistry and Sr-Nd-Pb isotopes
著者 (6件):
Li Wei
(Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China)
,
Tao Chunhui
(Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China)
,
Tao Chunhui
(School of Oceanography, Shanghai Jiao Tong University, Shanghai, China)
,
Liang Jin
(Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China)
,
Liao Shili
(Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China)
,
Yang Weifang
(Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China)
資料名:
International Geology Review
(International Geology Review)
巻:
62
号:
11
ページ:
1387-1405
発行年:
2020年
JST資料番号:
E0163C
ISSN:
0020-6814
CODEN:
IGREA
資料種別:
逐次刊行物 (A)
記事区分:
原著論文
発行国:
イギリス (GBR)
言語:
英語 (EN)