2008
DOI: 10.1038/nature07075
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Explosive volcanism on the ultraslow-spreading Gakkel ridge, Arctic Ocean

Abstract: Roughly 60% of the Earth's outer surface is comprised of oceanic crust formed by volcanic processes at mid-ocean ridges (MORs). Although only a small fraction of this vast volcanic terrain has been visually surveyed and/or sampled, the available evidence suggests that explosive eruptions are rare on MORs, particularly at depths below the critical point for

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Cited by 131 publications
(129 citation statements)
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“…8). All of them occur between 5 and 9 April 1999 and HYPOSAT places them in the central rift valley of Gakkel Ridge with events 1 and 3 being located extremely close to Oden volcano (Sohn et al 2008) and to each other (see Fig. 5).…”
Section: Cross-correlation Analysismentioning
confidence: 99%
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“…8). All of them occur between 5 and 9 April 1999 and HYPOSAT places them in the central rift valley of Gakkel Ridge with events 1 and 3 being located extremely close to Oden volcano (Sohn et al 2008) and to each other (see Fig. 5).…”
Section: Cross-correlation Analysismentioning
confidence: 99%
“…The lateral error of HYPOSAT at 95% confidence level is thus an underestimation of around 25%. All three events as laid out must reflect the same process to assume similar waveforms, all events are located between 12.6 to 16.4 km depth, all of them are located in the central rift valley, events 1 and 2 are indistinguishable up to 3,600 km offset from the source and events 1 and 3 plot nearly on the same spot close to Oden volcano (Sohn et al 2008). Thus, either this volcano or another vent aligned with Oden's chain of volcanoes and located further to the SE is the most probable source region for the repetitive events.…”
Section: Double-difference Locationmentioning
confidence: 99%
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