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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Published in | Earth and planetary science letters Vol. 333-334; pp. 52 - 62 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.06.2012
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Subjects | |
Online Access | Get full text |
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