2018
DOI: 10.1016/j.enggeo.2018.03.022
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Maintaining geological reality in application of GSI for design of engineering structures in rock

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Cited by 67 publications
(17 citation statements)
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“…In areas where rockmasses are particularly heterogeneous with multiple layers or zones of materials that exhibit distinct mechanical properties, successful variations of GSI to address these types of rockmass structure have been developed on a case by case basis. Examples of heterogeneous rockmasses for which GSI has been modified include tectonically disturbed interbedded sediments (Marinos and Hoek 2001;Marinos 2019), transition zones between fresh granite to residual soils (Babendererde et al 2004), ophiolite complexes with serpentinization (Marinos et al 2006), and other variability arising from tectonism, weathering, and alteration (Marinos and Carter 2018). This demonstrates the flexibility of GSI and supports the introduction of modifications to GSI for application to hydrothermally altered rockmasses with stockwork veins and other healed rockmass structures that are presented in this study.…”
Section: Applications Of Gsi To Heterogeneous Rockmassessupporting
confidence: 53%
“…In areas where rockmasses are particularly heterogeneous with multiple layers or zones of materials that exhibit distinct mechanical properties, successful variations of GSI to address these types of rockmass structure have been developed on a case by case basis. Examples of heterogeneous rockmasses for which GSI has been modified include tectonically disturbed interbedded sediments (Marinos and Hoek 2001;Marinos 2019), transition zones between fresh granite to residual soils (Babendererde et al 2004), ophiolite complexes with serpentinization (Marinos et al 2006), and other variability arising from tectonism, weathering, and alteration (Marinos and Carter 2018). This demonstrates the flexibility of GSI and supports the introduction of modifications to GSI for application to hydrothermally altered rockmasses with stockwork veins and other healed rockmass structures that are presented in this study.…”
Section: Applications Of Gsi To Heterogeneous Rockmassessupporting
confidence: 53%
“…Based on the H-B criterion, a series of estimation results of MPs corresponding to the IPs in the fluctuation ranges are obtainable, and then the sensitivity analyses of MPs to IPs can be carried out. e sensitivity function (S) and sensitivity factor (s i ) [22] used to describe the sensitivity relationships between IPs, MPs, and the predicted results of displacement and EDZ are defined as in (6) and (7)). To illustrate the physical meaning of s i , (7) is transformed into the expression, as shown in (8).…”
Section: Sensitivity Of the Mps Estimated By The H-b Criterion To Thementioning
confidence: 99%
“…Many methods have been proposed to solve the aforementioned difficulties. e method of converting rock parameters obtained by laboratory tests into engineering rock mass parameters, based on a rock mass classification system, has been increasingly recognized by specialists in the geotechnical engineering [6][7][8][9]. is method fully considers the integrated influence of joints and fissures in rock mass, groundwater, and size effects.…”
Section: Introductionmentioning
confidence: 99%
“…clearly characterised favoured failure surface or discontinuities. The appropriate use of rock mass characterisation systems, notably the GSI (for details, see [14,24]), allowed the quantification of difficult ground for the evaluation of the geotechnical properties and the selection of the design parameters. An extension of the original GSI application charts for heterogeneous and structurally complex rock masses, such as flysch, was initially introduced by Marinos and Hoek [10] and recently updated and extended by Marinos [11].…”
Section: Introductionmentioning
confidence: 99%
“…An extension of the original GSI application charts for heterogeneous and structurally complex rock masses, such as flysch, was initially introduced by Marinos and Hoek [10] and recently updated and extended by Marinos [11]. Specific GSI charts for molassic formations [12], ophiolites [13], gneiss in its disturbed form [14,15] and particular cases of limestones [15] and under particularly difficult geological conditions have been developed from experience gained during excavation of 62 tunnels as part of the Egnatia project in Northern Greece, along Alpine mountain belts.…”
Section: Introductionmentioning
confidence: 99%