Abstract
AN important question in submarine hydrothermal research concerns the connection between hydrothermal discharge from a spreading centre and variations in local magmatic and tectonic activity. Because it is likely that tectonic stretching and concomitant shallow magmatic activity triggered the cataclysmic venting that created the Juan de Fuca Ridge 'megaplumes'1–3, we have for three years monitored the 3He concentration and temperature anomaly of the underlying steady-state plume at the site of the original megaplume. We report here that the apparent 3He/heat ratio in the steady-state plume has progressively decreased from 4.4 to 2.4 to 1.3 x 10-12 cm3 STP cal-1 changing from a uniquely high ratio to one characteristic of established vent fields on other ridge segments4–8. We propose that the initially high 3He/heat ratio, sampled within days of the megaplume eruption, resulted from magma degassing into a hydrothermal circulation system of high permeability and short fluid residence time. Thus, high 3He/heat ratios may indicate venting created or profoundly perturbed by a magmatic–tectonic event, and lower ratios may typify systems at equilibrium.
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Baker, E., Lupton, J. Changes in submarine hydrothermal 3He/heat ratios as an indicator of magmatic/tectonic activity. Nature 346, 556–558 (1990). https://doi.org/10.1038/346556a0
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DOI: https://doi.org/10.1038/346556a0
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