Relationships between the microstructural evolution and the rheology of talc at elevated pressures and temperatures-Reference-Cited by-同舟云学术

Relationships between the microstructural evolution and the rheology of talc at elevated pressures and temperatures

Published:2008-04 Issue:3-4 Volume:268 Page:463-475
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Escartín J.,Andreani M.,Hirth G.,Evans B.

Publisher

Elsevier BV

Subject

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

Reference45 articles.

1. Andreani, M., Escartín, J., Hirth, G. & Evans, B. (2006), Deformation mode of talc from subsurface to dehydration conditions: implications for the subducting oceanic lithosphere, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract V31C-0599.

2. Occurrence and significance of serpentinite-hosted, talc-rich fault rocks in modern oceanic settings and ophiolite complexes;Boschi;Ofioliti,2006

3. Dilatancy in the fracture of crystalline rocks;Brace;J. Geophys. Res.,1966

4. Brittle–ductile transition in rocks;Byerlee;J. Geophys. Res.,1968

5. Rock-forming Minerals;Deer,1962

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