The Mixing Zephyr Pages
Are up flow
zones boundaries between adjacent hydrothermal systems? Geological and
geochemical tests
Mixing Zephyr Program
Endeavour Segment, Juan de Fuca Ridge
Summer 1995
Spatial variability in vent fluid chemistry
has been interpreted by ourselves and others as a result of a complex
series of processes related to phase separation and segregation within
the oceanic crust. This program examines an alternative hypothesis,
that the spatial patterns seen are related to the mixing of fluids
associated with two adjacent, independent hydrothermal convection
cells.
Funded by the National Science Foundation, NSF Grant OCE-9406965
Co-Investigators:
John
Delaney (Chief Scientist), Russ McDuff and Marv Lilley, University of Washington
Dave Butterfield and John Lupton, NOAA PMEL
These pages still have gaps...
- The Electronic Cruise Report
- A summary of at-sea
activity and primary data.
- Dive 3000
- During the second leg of the Mixing
Zephyr program, ALVIN Dive 3000 took place. Some of the festivities.
- Mapping Interface
- Form-based front end
to GMT routines for preparing track line maps.
- Ideas to Ponder
- Some memorable thoughts.
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These pages were last indexed on 3/28/96.
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The Mixing Zephyr Pages
Maintained by Russ McDuff (mcduff@ocean.washington.edu)
Copyright (©) 1995,1996 University of Washington; Copyright Notice
Content Last Modified 6/9/99
Page Last Built 6/9/99