Abstract: How the 410-km Discontinuity Reflects Mantle Water Content: Constraints from High-Pressure Experiments on Wadsleyite Single-Crystal Elasticity (2017 AGU Fall Meeting)

How the 410-km Discontinuity Reflects Mantle Water Content: Constraints from High-Pressure Experiments on Wadsleyite Single-Crystal Elasticity

Johannes Buchen¹, Hauke Marquardt², Tiziana Boffa Ballaran³, Takaaki Kawazoe², Sergio Speziale⁴ and Alexander Kurnosov³, (1)Bayerisches Geoinstitut, Universität Bayreuth, Bayreuth, Germany, (2)Bayerisches Geoinstitut, Universitaet Bayreuth, Bayreuth, Germany, (3)University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany, (4)Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany

Back to: Consequences of Mantle Phase Transitions I