Intragranular plasticity vs. grain boundary sliding (GBS) in forsterite: Microstructural evidence at high pressures (3.5–5.0 GPa)-Reference-Cited by-同舟云学术

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Intragranular plasticity vs. grain boundary sliding (GBS) in forsterite: Microstructural evidence at high pressures (3.5–5.0 GPa)

Published:2019-02-01 Issue:2 Volume:104 Page:220-231
ISSN:0003-004X
Container-title:American Mineralogist
language:en
Short-container-title:

Author:

Bollinger Caroline¹²,Marquardt Katharina¹³,Ferreira Filippe¹

Affiliation:

1. Bayerisches GeoInstitut, Universität Bayreuth, 95445 Bayreuth, Germany

2. † Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.

3. ‡ Department of Materials, Faculty of Engineering, Imperial College London, London, U.K.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

Link

https://pubs.geoscienceworld.org/msa/ammin/article-pdf/104/2/220/4628002/am-2019-6629.pdf

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