Chemical Nature of Hydrothermal Fluids Generated by Serpentinization and Carbonation of Komatiite: Implications for H 2 ‐Rich Hydrothermal System and Ocean Chemistry in the Early Earth-Reference-Cited by-同舟云学术

Chemical Nature of Hydrothermal Fluids Generated by Serpentinization and Carbonation of Komatiite: Implications for H 2 ‐Rich Hydrothermal System and Ocean Chemistry in the Early Earth

Published:2021-12 Issue:12 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Ueda Hisahiro¹^ORCID,Shibuya Takazo¹,Sawaki Yusuke²,Shozugawa Katsumi²^ORCID,Makabe Akiko¹,Takai Ken¹

Affiliation:

1. Super‐cutting‐edge Grand and Advanced Research (SUGAR) Program Institute for Extra‐cutting‐edge Science and Technology Avant‐garde Research (X‐star) Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka‐city Japan

2. Graduate School of Arts and Sciences The University of Tokyo Tokyo Japan

Funder

Ministry of Education, Culture, Sports, Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009827

Reference111 articles.

1. Length of the global plate boundary at 2.4 Ga

2. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars