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Measuring the Form of Iron in Hydrothermal Plume Particles

The global mid-ocean ridge (MOR) system is a 60,000 km submarine volcanic mountain range that crosses all of the major ocean basins on Earth. Along the MOR, subseafloor seawater circulation exchanges heat and elements between the oceanic crust and seawater. One of the elements released through this...

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Autors principals: Brandy M. Toner, Matthew A. Marcus, Katrina J. Edwards, Olivier Rouxel, Christopher R. German
Format: Artigo
Idioma:Inglês
Publicat: The Oceanography Society 2012-03-01
Col·lecció:Oceanography
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Accés en línia:http://tos.org/oceanography/archive/25-1_toner.pdf
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