Planes of Weakness and Their Patterns
Rock mass behavior, which for engineering purposes can be described by its resistance (strength), deformability, and permeability, is affected by the combined behavior of continuous (or intact) rock and the planes of weakness (discontinuities) (see Vol. XIII: Residual Stress, Rocks). Hereafter, planes of weakness will be called discontinuities , because such planes represent a rupture of the continuity of intact or solid rock. Discontinuities are planar features (or surfaces) of smaller resistance and higher deformability and permeability than the intact rock. This section describes the practical effects of these discontinuities, their geometric properties and their observation in the field.
Figure 1 shows practical effects of discontinuities in rock masses. Horizontal stress relief joints restrict the size of granite blocks that can be cut from the quarry in Fig. 1a. Horizontal bedding plane discontinuities weakened this shale block (Fig. 1b)...
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References
Billings, M. P., 1972, Structural Geology. Englewood Cliffs, N.J.: Prentice-Hall, 606 p.
Deere, D. U., A. H. Merritt, and R. F. Coon, 1969, Engineering classification of in-situ rock, U.S. Air Force Weapons Lab. Tech. Rept. No. AFWL-TR-67-144 or NTIS AD-848-798, 270 p.
Einstein, H. H., and C. H. Dowding, 1981, Shearing resistance and deformability of rock discontinuities, in Y. S. Touloukian, ed., Physical Properties of Rocks and Minerals. New York: McGraw-Hill, 177–219.
Goodman, R. E., 1980, Introduction to Rock Mechanics. New York: Wiley, 478 p.
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© 1988 Van Nostrand Reinhold Company Inc.
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Dowding, C.H. (1988). Fractures, fracture structures . In: General Geology. Encyclopedia of Earth Science. Springer, Boston, MA. https://doi.org/10.1007/0-387-30844-X_33
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DOI: https://doi.org/10.1007/0-387-30844-X_33
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