Messengers from the deep: Fossil wadsleyite-chromite microstructures from the Mantle Transition Zone

Investigations of the Mantle Transition Zone (MTZ; 410–660 km deep) by deformation experiments and geophysical methods suggest that the MTZ has distinct rheological properties, but their exact cause is still unclear due to the lack of natural samples. Here we present the first direct evidence for cr...

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Veröffentlicht in:	Scientific reports 2015-11, Vol.5 (1), p.16484-16484, Article 16484
Hauptverfasser:	Satsukawa, Takako, Griffin, William L., Piazolo, Sandra, O’Reilly, Suzanne Y.
Format:	Artikel
Sprache:	eng
Schlagworte:	704/2151/210 704/2151/213 704/2151/431 704/2151/536 Deformation Diffraction Dislocation Humanities and Social Sciences multidisciplinary Plastics Pressure Science Transition zone
Online-Zugang:	Volltext
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