Kilometre-scale thermohaline overturn of pore waters in the Louisiana Gulf Coast

Geochemical and physical evidence for the existence of density inversions in Gulf Coast pore fluids sufficient to drive large-scale convective fluid flow at rates conceivably as high as metres per year is presented.

Bibliographic Details

Published in:	Nature (London) 1987-06, Vol.327 (6122), p.501-503
Main Author:	Hanor, Jeffrey S
Format:	Article
Language:	English
Subjects:	Applied sciences Exact sciences and technology Oceans Other techniques and industries Water
Citations:	Items that cite this one
Online Access:	Get full text
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