Transformation microstructures in pyrolite under stress: Implications for anisotropy in subducting slabs below the 660 km discontinuity

Author:

Gay Jeffrey P.ORCID,Ledoux Estelle,Krug MatthiasORCID,Chantel JulienORCID,Pakhomova Anna,Liermann Hanns-PeterORCID,Sanchez-Valle Carmen,Merkel SébastienORCID

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference71 articles.

1. The deformational journey of the Nazca slab from seismic anisotropy;Agrawal;Geophys. Res. Lett.,2020

2. Detailed nature of the 660 km region of the mantle from global receiver function data;Andrews;J. Geophys. Res., Solid Earth,2008

3. Texture analysis with MTEX-Free and open source software toolbox;Bachmann,2010

4. Radial anisotropy in seismic reference models of the mantle;Beghein;J. Geophys. Res., Solid Earth,2006

5. Probing depth and lateral variations of upper-mantle seismic anisotropy from full-waveform inversion of teleseismic body-waves;Beller;Geophys. J. Int.,2020

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