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...

Full description

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

Internet

http://hdl.handle.net/1721.1/118477
https://orcid.org/0000-0002-1348-9584

Similar Items