2013
DOI: 10.7424/jsm130407
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High Temperature Versus Geomechanical Parameters of Selected Rocks – The Present State of Research

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Cited by 52 publications
(24 citation statements)
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“…In a similar manner to strength, the elastic response of rock depends mainly on the elastic properties of the constituent minerals, the degree of cementation and porosity (Sygała et al 2013). Under the influence of high temperatures, another important factor that affects rock strength and elastic response is the thermal expansion of the constituent minerals.…”
Section: Micro-ct Resultsmentioning
confidence: 99%
“…In a similar manner to strength, the elastic response of rock depends mainly on the elastic properties of the constituent minerals, the degree of cementation and porosity (Sygała et al 2013). Under the influence of high temperatures, another important factor that affects rock strength and elastic response is the thermal expansion of the constituent minerals.…”
Section: Micro-ct Resultsmentioning
confidence: 99%
“…() and Sygala et al. () showed that at 600–1200 °C, depending on rock type, Young's moduli drop to 10–66% of their surface value. We therefore calculated thermal stresses using Young's moduli covering the range between 15 and 60 GPa.…”
Section: Emplacement Mechanisms For Qd and Miqd Dykesmentioning
confidence: 97%
“…Temperature is one factor that can alter the physical properties in rock. As temperature increases, thermal expansion of rockforming minerals weakens the rock mass and may cause its destruction (Dimitriyev et al 1969;Heuze 1983;Somerton 1992;Den'gina et al 1994;Hajpál and Török 2004;Sygała et al 2013;Cieślik 2015). Changes in physical rock properties under high temperatures may have a practical impact on in situ mining deposits, as well as creating issues for mine safety.…”
Section: Introductionmentioning
confidence: 99%
“…However, datasets are wide-ranging, and it is difficult to characterize uniformly the behavior of rocks under high Editorial handling: Pinnaduwa Kulatilake temperatures. The thermal influence on the behavior of rocks is closely dependent on the heating conditions, rock type, mineralogy, distribution of microfissures and primary cracks, density, porosity, and many other factors (Chaki et al 2008;Keshavarz et al 2010;Sygała et al 2013).…”
Section: Introductionmentioning
confidence: 99%