Geochemistry of fluids from Earth’s deepest ridge-crest hot-springs: Piccard hydrothermal field, Mid-Cayman Rise

Geochemistry of fluids from Earth’s deepest ridge-crest hot-springs: Piccard hydrothermal field, Mid-Cayman Rise

Hosted in basaltic substrate on the ultra-slow spreading Mid-Cayman Rise, the Piccard hydrothermal field is the deepest currently known seafloor hot-spring (4957–4987 m). Due to its great depth, the Piccard site is an excellent natural system for investigating the influence of extreme pressure on th...

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Bibliographic Details
Main Authors:	McDermott, Jill M., Sylva, Sean P., Ono, Shuhei, German, Christopher R., Seewald, Jeffrey S.
Other Authors:	Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format:	Article
Published:	Elsevier BV 2018
Online Access:	http://hdl.handle.net/1721.1/118477 https://orcid.org/0000-0002-1348-9584

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