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Did the formation of Dʺ; cause the Archaean-Proterozoic transition?

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dc.contributor.authorCampbell, Ian
dc.contributor.authorGriffiths, Ross
dc.date.accessioned2015-12-13T22:37:55Z
dc.date.issued2014
dc.date.updated2015-12-11T09:39:15Z
dc.description.abstractThe MgO content of the highest MgO plume-related komatiites and picrites remained constant at 32 ± 2.5% between 3.5 and 2.7 Ga, then fell to 21 ± 3% by ca. 2.0 Ga, a value similar to the present day value. Because there is a linear relationship between
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/77311
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.titleDid the formation of Dʺ; cause the Archaean-Proterozoic transition?
dc.typeJournal article
local.bibliographicCitation.lastpage8
local.bibliographicCitation.startpage1
local.contributor.affiliationCampbell, Ian, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationGriffiths, Ross, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidCampbell, Ian, u8300206
local.contributor.authoruidGriffiths, Ross, u8300081
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040402 - Geodynamics
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB6203
local.identifier.citationvolume388
local.identifier.doi10.1016/j.epsl.2013.11.048
local.identifier.scopusID2-s2.0-84890226658
local.identifier.thomsonID000331502600001
local.type.statusPublished Version

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