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Testing the plume theory

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dc.contributor.authorCampbell, Ian
dc.date.accessioned2015-12-07T22:52:24Z
dc.date.issued2007
dc.date.updated2015-12-07T12:29:07Z
dc.description.abstractThe physics of low Reynolds number plumes is well understood, and this allows a number of testable predictions to be made about mantle plumes. Mantle plumes are predicted to originate from the core-mantle boundary and consist of a large head, ∼ 1000 k
dc.identifier.issn0009-2541
dc.identifier.urihttp://hdl.handle.net/1885/27421
dc.publisherElsevier
dc.sourceChemical Geology
dc.subjectKeywords: boundary layer; core-mantle boundary; crustal thickening; flood basalt; frequency-magnitude distribution; large igneous province; mantle plume; numerical model; oceanic crust; prediction; seismic method; spreading center; uplift; volcanism; Arctic; Atlant Flood basalt; Mantle plumes; Picrites; Uplift
dc.titleTesting the plume theory
dc.typeJournal article
local.bibliographicCitation.lastpage176
local.bibliographicCitation.startpage153
local.contributor.affiliationCampbell, Ian, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidCampbell, Ian, u8300206
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040303 - Geochronology
local.identifier.ariespublicationu4047674xPUB51
local.identifier.citationvolume241
local.identifier.doi10.1016/j.chemgeo.2007.01.024
local.identifier.scopusID2-s2.0-34249821898
local.type.statusPublished Version

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