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Influence of grain size and geothermal gradient on the ductile-to-brittle transition in arenaceous sedimentary rocks: implications for fault structure and fluid flow

✍ Scribed by Fisher, Q. J.; Harris, S. D.; Casey, M.; Knipe, R. J.


Book ID
126688570
Publisher
The Geological Society (London)
Year
2007
Tongue
English
Weight
875 KB
Volume
289
Category
Article
ISSN
0305-8719

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