Autor: |
Peter J. Schultheiss, Marcus G. Langseth, Keir Becker, Richard P. Von Herzen |
Rok vydání: |
1992 |
Předmět: |
|
Zdroj: |
Geophysical Research Letters. 19:517-520 |
ISSN: |
0094-8276 |
DOI: |
10.1029/92gl00079 |
Popis: |
A comprehensive survey of heat flow, sediment thickness and bathymetry in a large intermontane sediment pond on the western flank of the Mid-Atlantic Ridge (North Pond) shows that only 20 to 25% of the heat escaping from the lithosphere flows through the sediments in the pond even though they completely cover a 70 km2 area of the seafloor. Three in situ pore-pressure gradient measurements gave values that were negative relative to hydrostatic, indicating that there is drawdown of water through the sediment at rates of 1 to 5 mm/yr. North Pond is a recharge zone for hydrothermal circulation that is probably driven by lateral pressure gradients produced by topographic relief. |
Databáze: |
OpenAIRE |
Externí odkaz: |
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