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dc.contributor.authorHagen, R.A.
dc.contributor.authorGohl, K.
dc.contributor.authorGersonde, R.
dc.contributor.authorKuhn, G.
dc.contributor.authorVolker, D.
dc.contributor.authorKodagali, V.N.
dc.date.accessioned2008-02-22T05:31:28Z
dc.date.available2008-02-22T05:31:28Z
dc.date.issued1998
dc.identifier.citationGeo-Marine Letters, Vol.18(1); 19-25p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/969
dc.description.abstractThe De Gerlache Seamounts actually consist of two medium-sized guyots, with summits at depths of 350-600 m. Acoustic profiler data show no significant sediment on these guyots. Alkaline basalts dredged from the summit of the eastern guyot yield K/Ar ages between 20.1 ~c 1.0 and 23.2 ~c 1.2 Ma. Basement ridges and sediment-filled troughs between the guyots are associated with the prominent gravity anomaly extending north from the Antarctic margin. This structure possibly played a role in the guyot formation, however, the question of how the De Gerlache Seamounts are related to this gravity anomaly remains uncertain.
dc.language.isoen
dc.publisherSpringer
dc.rightsCopyright [1998]. It is tried to respect the rights of the copyright holders to the best of the knowledge. If it is brought to our notice by copyright holder that the rights are voilated then the item would be withdrawn.
dc.subjectSeamounts
dc.subjectsediments
dc.titleA geophysical survey of the De Gerlache Seamounts: Preliminary results
dc.typeJournal Article


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