Iron isotopes constrain sub-seafloor hydrothermal processes at the Trans-Atlantic Geotraverse (TAG) active sulfide mound

Iron isotopes constrain sub-seafloor hydrothermal processes at the Trans-Atlantic Geotraverse (TAG) active sulfide mound

Iron isotopic equilibration at the Trans-Atlantic Geotraverse hydrothermal field takes place over tens of thousands of years, with variable degrees of hydrothermal maturation throughout the active mound, according to iron isotope analyses of sulfide minerals.

Bibliographic Details
Main Authors: Fredrik Sahlström, Valentin R. Troll, Sabina Strmić Palinkaš, Ellen Kooijman, Xin-Yuan Zheng
Format: Article
Language:English
Published: Nature Portfolio 2022-08-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-022-00518-2

Internet

https://doi.org/10.1038/s43247-022-00518-2

Similar Items