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
Author:
Affiliation:
1. Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
2. School of Oceanography, Shanghai Jiao Tong University, Shanghai, China
Funder
China Postdoctoral Science Foundation
China Ocean Mineral R&D Association (COMRA) Major project
National Key R&D Program of China
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2019.1647467
Reference74 articles.
1. Petrology of Lavas from the Lamont Seamount Chain and Adjacent East Pacific Rise, 10 N
2. Implications of a two-component marble-cake mantle
3. Chemical variations and regional diversity observed in MORB
4. Do We Really Need Mantle Components to Define Mantle Composition?
5. Chemical and isotopic variations along the superfast spreading East Pacific Rise from 6 to 30�S
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