Paleointensity applications to timing and extent of eruptive activity, 9°–10°N East Pacific Rise

dc.creatorBowles, Julie A.
dc.creatorGee, Jeffrey S.
dc.creatorKent, Dennis V.
dc.creatorPerfit, Michael R.
dc.creatorSoule, S. Adam
dc.creatorSoule, S. Adam
dc.date.accessioned2024-12-06T19:25:02Z
dc.date.available2024-12-06T19:25:02Z
dc.date.issued2006-06-08
dc.description.abstractPlacing accurate age constraints on near-axis lava flows has become increasingly important given the structural and volcanic complexity of the neovolcanic zone at fast spreading ridges. Geomagnetic paleointensity of submarine basaltic glass (SBG) holds promise for placing quantitative age constraints on near-axis flows. In one of the first extensive tests of paleointensity as a dating tool or temporal marker we present the results of over 550 successful SBG paleointensity estimates from 189 near-axis (
dc.identifier.urihttp://digital.library.wisc.edu/1793/84996
dc.relation.replaceshttps://dc.uwm.edu/geosci_facart/2
dc.subjectPaleointensity
dc.subjectPaleomagnetism applied to geologic processes
dc.subjectMidocean ridge processes
dc.titlePaleointensity applications to timing and extent of eruptive activity, 9°–10°N East Pacific Rise
dc.typearticle

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