Talc-dominated seafloor deposits reveal a new class of hydrothermal system

The Von Damm Vent Field (VDVF) is located on the flanks of the Mid-Cayman Spreading Centre, 13 km west of the axial rift, within a gabbro and peridotite basement. Unlike any other active vent field, hydrothermal precipitates at the VDVF comprise 85–90% by volume of the magnesium silicate mineral, ta...

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Detalles Bibliográficos
Autores principales: Hodgkinson, Matthew R. S., Webber, Alexander P., Roberts, Stephen, Mills, Rachel A., Connelly, Douglas P., Murton, Bramley J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4703833/
https://www.ncbi.nlm.nih.gov/pubmed/26694142
http://dx.doi.org/10.1038/ncomms10150

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4703833/
https://www.ncbi.nlm.nih.gov/pubmed/26694142
http://dx.doi.org/10.1038/ncomms10150

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