Characterisation of hydrothermal sediments at the TAG hydrothermal field (MAR, 26°N) and metal mobilisation in interstitial fluids

Adeline DutrieuxNational Oceanography Centre, University of Southampton, Southampton, United KingdomCorrespondence[email protected]

Anna LichtschlagNational Oceanography Centre, Natural Environment Research Council, Southampton, United Kingdom

Bramley MurtonNational Oceanography Centre, Natural Environment Research Council, Southampton, United Kingdom

Reference

Goulding HC, Mills RA, Nesbit RW. 1998. Precipitation of hydrothermal sediments on the active TAG mound: implications for ochre formation. In: Mills RA, Harrisson K, editors. Modern ocean floor processes and the geological record. London: Geological Society, Special Publications, 148; p. 201–216.
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Severmann S, Mills RA, Palmer M, Fallick A. 2004. The origin of clay minerals in active and relict hydrothermal deposits. Geochim Cosmochim Ac. 68:73–88. doi: 10.1016/S0016-7037(03)00235-7
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Characterisation of hydrothermal sediments at the TAG hydrothermal field (MAR, 26°N) and metal mobilisation in interstitial fluids

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Characterisation of hydrothermal sediments at the TAG hydrothermal field (MAR, 26°N) and metal mobilisation in interstitial fluids

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