Physics – Geophysics
Scientific paper
Jul 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994e%26psl.125..119m&link_type=abstract
Earth and Planetary Science Letters (ISSN 0012-821X), vol. 125, no. 1-4, p. 119-128
Physics
Geophysics
22
Atlantic Ocean, Geothermal Resources, Hydrothermal Systems, Imaging Techniques, Mid-Ocean Ridges, Ocean Bottom, Ocean Data Acquisitions Systems, Sea Floor Spreading, Sulfides, Geochemistry, Geophysics
Scientific paper
A survey along the axis of the slow-spreading Mid-Atlantic Ridge, between 27 deg N and 30 deg N, using a combination of geophysical imaging and geochemical sensing has assessed the regional extent of hydrothermal activity. As a result, three areas were identified as possible sources of hydrothermal activity: at 27 deg 00 min N, 29 deg 10 min N and 30 deg 02 min N. The location of the strongest signals of high-temperature activity, at 29 deg 10 min N, was examined with a combination of water column sensors and sea floor observations, including submersible studies. These studies confirmed the presence of a high-temperature hydrothermal vent field comprising three discrete 'black smoker' sources of fluid in excess of 350 C, as well as two weathered sulfide mounds with diffuse, low-temperature fluid seeps. This systematic regional survey of the Mid-Atlantic Ridge reinforces the earlier supposition that hydrothermal activity is spatially restricted on slow spreading ridges in comparison to fast spreading ridges.
Becker Klaus
Briais Anne
Edge David
Hayward Nick
Klinkhammer Gary
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