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Definition
Shale is a fine-grained, siliciclastic, laminated sedimentary rock composed mainly of indurated silt and clay size particles of clay minerals, fine-size quartz, and feldspars.
Characteristics
Shale is the most frequently encountered rock in engineering projects associated with sedimentary basins. Sedimentary basins, having low water energy, provide suitable conditions for deposition of fine-grained suspended particles to form shale. The presence of fissility, the ability of a rock to readily split into thin pieces with a maximum thickness of 10 mm, along the laminations (Czerewko and Cripps 2012) is the key indicator to distinguish shale from other mudrocks such as mudstone and claystone. The predominant grain size of shale is smaller than 0.063 mm. In addition to clay minerals, fine-size quartz and feldspars, carbonate minerals (calcite, dolomite), pyrite, heavy minerals, and...
References
Czerewko MA, Cripps JC (2012) Mudrocks, clays and pyrite. In: ICE manual of geotechnical engineering, pp 481–516
Dick JC, Shakoor A, Wells N (1994) A geological approach toward developing a mudrock-durability classification system. Can Geotech J 31:17–27
Fisher Q, Kets F, Crook A (2013) Self-sealing of faults and fractures in argillaceous formations: evidence from the petroleum industry. NAB 13-06
Freeze RA, Cherry JS (1979) Groundwater. Prentice-Hall, Englewood Cliffs, 604 p.
Steiger RP, Leung PK (1992) Quantitative determination of the mechanical properties of shales. SPE Drill Eng 7(3): 181–185, Society of Petroleum Engineers
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Erguler, Z.A. (2016). Shale. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_255-1
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DOI: https://doi.org/10.1007/978-3-319-12127-7_255-1
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