Olivine rheology, shear stress, and grain growth in the lithospheric mantle: Geological constraints from the Kaapvaal craton

The rheology of Earth's mantle is a complex function that depends on, at least, temperature, pressure, stress, grain size, and water content. Understanding this functionality is of fundamental importance in mantle dynamics, but constraints from laboratory experiments entail considerable extrapo...

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Bibliographic Details
Published inEarth and planetary science letters Vol. 333-334; pp. 52 - 62
Main Authors Chu, Xu, Korenaga, Jun
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2012
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