Penetrative Convection in Earth's Mantle : a Test Using Whole-Earth Geochemical Model.

dc.contributor.advisorIhinger, Phillip D.
dc.contributor.authorUlrich, Sarah A.
dc.date.accessioned2009-07-23T15:02:48Z
dc.date.available2009-07-23T15:02:48Z
dc.date.issued2009-07-23T15:02:48Z
dc.descriptionColor poster with text, images, and graphs (Spring 2009)en
dc.description.abstractThe nature of mantle convection within the Earth remains one of the most important unanswered questions regarding Earth evolution. Two competing theories have been proposed; one backed primarily by geochemists invoking two separately convecting homogeneous upper and lower reservoirs, and the other backed primarily by geophysicists invoking a single incompletely stirred reservoir. The recently proposed Penetrative Convection Model offers a reconciliation of the two perspectives. Here we present whole-Earth geochemical models that apply the dynamics of the Penetrative Convection Model and follow the geochemical evolution of the upper and lower mantles.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programs. Petroleum Research Fund.en
dc.identifier.urihttp://digital.library.wisc.edu/1793/35586
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectEarth--Evolutionen
dc.subjectEarth--Mantle--Modelsen
dc.subjectHeat--Convection--Modelsen
dc.subjectPostersen
dc.subjectTerrestrial heat flow--Modelsen
dc.titlePenetrative Convection in Earth's Mantle : a Test Using Whole-Earth Geochemical Model.en
dc.typePresentationen

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