Fluid flow and heat transport in the upper continental crust

D Deming - Geological Society, London, Special Publications, 1994 - lyellcollection.org
The upper 10–15km of the continental crust is saturated with aqueous brines and is
sufficiently permeable to allow the circulation of these fluids. The most important driving …
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[引用][C] Fluid flow and heat transport in the upper continental crust

D Deming - Geological Society of London Special …, 1994 - ui.adsabs.harvard.edu
Fluid flow and heat transport in the upper continental crust - NASA/ADS Now on home page
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