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Stress-induced Magnetic Anisotropy of Rocks

✍ Scribed by STACEY, F. D.

Book ID
109611443
Publisher
Nature Publishing Group
Year
1960
Tongue
English
Weight
314 KB
Volume
188
Category
Article
ISSN
0028-0836

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Anisotropic stress states are common in the upper crust and result in fracture apertures being dependent on fracture orientation. Fractured rocks should therefore display an anisotropic permeability determined by the aperture, length, and orientation of those fractures remaining open. In this paper,