Iron Oxyhydroxide‐Rich Hydrothermal Deposits at the High‐Temperature Fåvne Vent Field, Mohns Ridge

Abstract The recently discovered Fåvne vent field, located at 3,040 m depth on the slow‐spreading Mohns mid‐ocean ridge between Greenland and Norway, is a high‐temperature (≥250°C) vent field that is characterized by Fe oxyhydroxide‐rich and S‐poor chimneys and mounds. The vent field is located on b...

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Egile Nagusiak:	Caroline Gini, John W. Jamieson, Eoghan P. Reeves, Amy Gartman, Thibaut Barreyre, Michael G. Babechuk, Steffen L. Jørgensen, Katleen Robert
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Wiley 2024-06-01
Saila:	Geochemistry, Geophysics, Geosystems
Gaiak:	major and trace element geochemistry sedimentary geochemistry hydrothermal systems mid‐oceanic ridge processes mineral occurrences and deposits
Sarrera elektronikoa:	https://doi.org/10.1029/2024GC011481
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