The stabilisation and transportation of dissolved iron from high temperature hydrothermal vent systems-Reference-Cited by-同舟云学术

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The stabilisation and transportation of dissolved iron from high temperature hydrothermal vent systems

Published:2013-08 Issue: Volume:375 Page:280-290
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Hawkes J.A.,Connelly D.P.,Gledhill M.,Achterberg E.P.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference101 articles.

1. A method for quantitatively estimating diffuse and discrete hydrothermal discharge;Baker;Earth Planet. Sci. Lett.,1993

2. Hydrothermal activity and volcano distribution along the Mariana Arc;Baker;J. Geophys. Res.-Solid Earth,2008

3. Characteristics of hydrothermal plumes from 2 vent fields on the Juan-de-Fuca ridge, Northeast Pacific Ocean;Baker;Earth Planet. Sci. Lett.,1987

4. The distribution and stabilisation of dissolved Fe in deep-sea hydrothermal plumes;Bennett;Earth Planet. Sci. Lett.,2008

5. Dissolved and particulate organic carbon in hydrothermal plumes from the East Pacific Rise, 9 degrees 50°N;Bennett;Deep-Sea Res. Part I-Oceanogr. Res. Pap.,2011

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