1995
DOI: 10.1016/0013-7952(95)00055-0
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Engineering geological characterization of low strength anisotropic rocks in the Himalayan region for assessment of tunnel support

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Cited by 26 publications
(5 citation statements)
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“…Therefore, joint directions of the rocks could not be further studied. (Bhasin et al, 1995;Desai and Salami, 1987;Gurocak et al, 2012;Saroglou et al, 2004;Shea Jr and Kronenberg, 1993;Yilmaz, 2009) or prismatic specimens (Ramamurthy et al, 1993;Singh et al, 2002;Tiwari and Rao, 2007). As a result of the challenges in obtaining natural intact rock cores of suitable lengths, and also due to the friability of the in-situ rock, it was not practically possible to ascertain the anisotropy of the rock mass.…”
Section: Proposed Methods Of Testing Reconstituting Rock Spoilsmentioning
confidence: 99%
“…Therefore, joint directions of the rocks could not be further studied. (Bhasin et al, 1995;Desai and Salami, 1987;Gurocak et al, 2012;Saroglou et al, 2004;Shea Jr and Kronenberg, 1993;Yilmaz, 2009) or prismatic specimens (Ramamurthy et al, 1993;Singh et al, 2002;Tiwari and Rao, 2007). As a result of the challenges in obtaining natural intact rock cores of suitable lengths, and also due to the friability of the in-situ rock, it was not practically possible to ascertain the anisotropy of the rock mass.…”
Section: Proposed Methods Of Testing Reconstituting Rock Spoilsmentioning
confidence: 99%
“…It is typically necessary to have intact rock core lengths or prismatic specimens in order to proceed with rock strength tests, such as the uniaxial compression strength test, point load test, Brazilian tensile test, triaxial test or shear wave velocity test (Bhasin et al, 1995;Gurocak et al, 2012;Ramamurthy et al, 1993;Saroglou et al, 2004;Shea and Kronenberg, 1993;Tiwari and Rao, 2007). However, the highly fractured Tuang Formation meant that it was difficult to attain sound rock core lengths, which subsequently created challenges in measuring the rock strength parameters.…”
Section: Introductionmentioning
confidence: 99%
“…In situ stresses along the tunnel route have been measured by hydraulic fracturing and by overcoring techniques (Bhasin et al 1996). The following values were found for the principal stresses: cy~ =7.1 MPa, approximately parallel to valley cy2 = 5.9 MPa, vertical stress cL~=3.9 MPa, approximately normal to valley However, because of the general weakness of the rock mass in the region of the Daj Khad shear zone, it has been assumed that the rock mass cannot tolerate significant stress differences and that all three principal in situ stresses are equal.…”
Section: Practical Examplementioning
confidence: 99%