Flow of synthetic, wet, partially molten “granite” under undrained conditions: An experimental study-Reference-Cited by-同舟云学术

Flow of synthetic, wet, partially molten “granite” under undrained conditions: An experimental study

Published:2006-06 Issue:B6 Volume:111 Page:n/a-n/a
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Rutter E. H.¹,Brodie K. H.¹,Irving D. H.¹

Affiliation:

1. Rock Deformation Laboratory, School of Earth, Atmospheric and Environmental Sciences; University of Manchester; Manchester UK

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference45 articles.

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3. The temperature and strain rate dependent behaviour of a polycrystalline galena ore;Atkinson;Econ. Geol.,1976

4. Steady-state creep of fine grain granite at partial melting;Auer;J. Geophys.,1981

5. Work hardening and recovery during compressive creep;Birch;J. Mater. Sci.,1974

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