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Permeability of the continental crust: implications of experimental data
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DOI：10.1016/S0375-6742(03)00129-8.png)
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Abstract
En 中文
We suggest a correlation of the crustal rocks' permeability with depth based on the original experimental data. The analytical expression for the trend is given by log k= - 12.56-3.225H(0.223), where k is in square meters and H is in kilometers. The permeability decreases from 2.75 x 10(-13+/-1.9) m(2) at the surface to 1.67 x 10(-20 +/- 1.5) m(2) at the base of the crust. (C) 2003 Published by Elsevier Science B.V.
Keywords:
permeability
continental crust
experiment
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3.3
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