Variation in the Permeability of Intact and Fractured Rocks due to Transient Disturbances in Axial Stress or Pore Pressure

<table class="table-group" id="tab2"><tr><td><table class="table"><tr><td class="thead-hr" colspan="8"><hr/></td></tr><tr class="thead"><td class="align_left">Qz</td><td class="align_center">Pl</td><td class="align_center">Kf</td><td class="align_center">Am</td><td class="align_center">Hm</td><td class="align_center">Mc</td><td class="align_center">Chl</td><td class="align_center">Sm</td></tr><tr><td class="thead-hr" colspan="8"><hr/></td></tr><tr><td class="align_left">Very abundant</td><td class="align_center">Very abundant</td><td class="align_center">Abundant</td><td class="align_center">Very little</td><td class="align_center">Little</td><td class="align_center">Little</td><td class="align_center">Little</td><td class="align_center">Medium</td></tr><tr class="table-tr"><td colspan="8"><hr class="tbody-hr"/></td></tr></table></td></tr><tr class="table-fn"><td><div>Qz: quartz; Pl: plagioclases; Kf: potash feldspar; Am: amphibole; Hm: hematite; Mc: mica; Chl: chlorite; Sm: smectite.<br/></div></td></tr></table>

<div>Mineral composition of the Kushiro Cretaceous sandstone from XRD analysis.</div>

Advances in Civil Engineering

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Table 2

Table 2: Variation in the Permeability of Intact and Fractured Rocks due to Transient Disturbances in Axial Stress or Pore Pressure 