Diffusion Creep and Grain Growth in Forsterite +20 vol% Enstatite Aggregates: 1. High-Resolution Experiments and Their Data Analyses-Reference-Cited by-同舟云学术

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Diffusion Creep and Grain Growth in Forsterite +20 vol% Enstatite Aggregates: 1. High-Resolution Experiments and Their Data Analyses

Published:2018-11 Issue:11 Volume:123 Page:9486-9512
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Nakakoji T.¹,Hiraga T.¹^ORCID,Nagao H.¹²^ORCID,Ito S.¹,Kano M.³^ORCID

Affiliation:

1. Earthquake Research Institute; The University of Tokyo; Tokyo Japan

2. Department of Mathematical Informatics, Graduate School of information Science and Technology; The University of Tokyo; Tokyo Japan

3. Department of Geophysics, Graduate School of Science; Tohoku University; Sendai Japan

Funder

Japan Society for the Promotion of Science

Earthquake Research Institute's cooperative research program

Ministry of Education, Culture, Sports, Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

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

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JB015818/fullpdf

Reference43 articles.

1. Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman-UAE ophiolite;Ambrose;Earth and Planetary Science Letters,2018

2. On the coarsening of grain boundary precipitates;Ardell;Acta Metallurgica,1972

3. Interface controlled diffusional creep;Arzt;Acta Metallurgica,1983

4. Diffusion-accommodated flow and superplasticity;Ashby;Acta Metallurgica,1973

5. Inverse problems in stochastic modeling of mixed-mode power-law and diffusional creep for distributed grain size;Bai;Metallurgical and Materials Transactions A,2010

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4. Relation between rheological properties and the stress state in subducting slabs;Earth, Planets and Space;2024-01-09

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