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; Uehara, Shinichi*; *; *
American Geophysical Union 2002 Fall Meeting, p.F1371 - F1372, 2002/12
The effect of micro-cracks on the transport properties of granite is studied using laser scanning microscope. 3D images of pore structure show the influence on the porosity and permeability. Anisotropy of micro-cracks are observed on two different directions in respect to the main structure. Results on permeability show a decreases by a factor of one to two order of magnitude in the direction parallel to the fault zone. In the conference will be discussed the implications of anisotropy of micro-cracks on the transport properties in crystalline rocks.
Deformation Mechanisms, Rheology and Techonics, P. 125, 2001/00
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