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Hydraulic Fracturing in Geological Processes: A Review

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Hydraulic fracturing and geothermal energy

Part of the book series: Mechanics of elastic and inelastic solids ((MEIS,volume 5))

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Abstract

In the Earth’s crust there occur many emplacement bodies and fissure-filling columns, such as salt plugs, igneous stocks, sheet intrusions, clastic dikes, and mineral veins. Since they were formed with relation to the activity of some fluid materials, such as plastic salt, magma, water, aqueous solution, they may be analogs of hydraulic fractures. With the increase of pore-pressure, rocks become weak and also brittle even under a relatively high confining pressure. This implies that the pore-pressure affects the fracture pattern as well as the strength of rocks.

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© 1983 Martinus Nijhoff Publishers, The Hague

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Shoji, T., Takenouchi, S. (1983). Hydraulic Fracturing in Geological Processes: A Review. In: Nemat-Nasser, S., Abé, H., Hirakawa, S. (eds) Hydraulic fracturing and geothermal energy. Mechanics of elastic and inelastic solids, vol 5. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-6884-4_11

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  • DOI: https://doi.org/10.1007/978-94-009-6884-4_11

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-009-6886-8

  • Online ISBN: 978-94-009-6884-4

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