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Origins of Si-Fe cap rocks at extinct seafloor massive sulphide (eSMS) deposits: an example from the ALVIN Zone in the TAG Hydrothermal Field (26°), Mid-Atlantic Ridge.
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Stobbs, I. J., Murton, B. J., Pearce, R., Boyce, A. and Petersen, Sven (2019) Origins of Si-Fe cap rocks at extinct seafloor massive sulphide (eSMS) deposits: an example from the ALVIN Zone in the TAG Hydrothermal Field (26°), Mid-Atlantic Ridge. [Talk] In: 15. Biennal SGA Meeting. , 27.-30.08.2019, Glasgow, UK ; pp. 91-94 .
Full text not available from this repository.Document Type: | Conference or Workshop Item (Talk) |
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Additional Information: | Proceedings of the 15th Biennal SGA Meeting, pp. 91 - 94 |
Research affiliation: | OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems > FB4-MUHS Marine Mineralische Rohstoffe OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems |
Date Deposited: | 10 Oct 2019 12:14 |
Last Modified: | 10 Oct 2019 12:14 |
URI: | https://oceanrep.geomar.de/id/eprint/47897 |
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