Formation of hydrothermal ferromanganese oxides from the Daigo-Kume Knoll in the middle Okinawa Trough, Japan-Reference-Cited by-同舟云学术

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Formation of hydrothermal ferromanganese oxides from the Daigo-Kume Knoll in the middle Okinawa Trough, Japan

Published:2023-09 Issue: Volume:463 Page:107117
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Azami Keishiro,Koyama Kanta,Machida Shiki,Okino Kyoko,Yasukawa Kazutaka,Kato Yasuhiro,Uchida Etsuo

Funder

National Institute of Advanced Industrial Science and Technology

National Museum of Nature and Science

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference74 articles.

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2. Release of Ni from birnessite during transformation of birnessite to todorokite: implications for Ni cycling in marine sediments;Atkins;Geochim. Cosmochim. Acta,2016

3. Rare earth elements and yttrium (REY) variability with water depth in hydrogenetic ferromanganese crusts;Azami;Chem. Geol.,2018

4. Hydrothermal ferromanganese oxides around a petit-spot volcano on old and cold oceanic crust;Azami;Commun. Earth Environ.,2023

5. Rare-earth element mobility during hydrothermal and metamorphic fluid rock interaction and the significance of the oxidation-state of europium;Bau;Chem. Geol.,1991

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Formation of hydrothermal ferromanganese oxides in the Daini-Nishi-Yamato Seamount, Sea of Japan: Do they really contain critical-metal particles?;Ore Geology Reviews;2024-09

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