Engineering Geology

Engineering Geology

Investigation of the effect of mineralogy in strenghth of schist rocks in Mouteh gold mine

Abstract
In this study, due to the landslide in schist rocks, in the wall of Mouteh gold mines, including of the eastern wall of ChahKhatoon mine, it is important to identify the effective factors. Therefore, due to the diversity of schists in Chah Khatoon and Sanjadeh gold mines (two active mines in Mouteh Complex), to survey the mineralogy of schist rocks in Moteh gold mine has been done by identifying important factors in changes in rock strength. Cosequently, 10 schist samples from walls of these mines were considered for mineralogical, XRD studies. In the next step, these schists were subjected to uniaxial compressive strength (UCS) and Brazilian tests to estimate the mechanical properties and quality of rock mass in different zones of mineral walls. The results showed that the UCS and Brazilian index in these schists are directly and inversely related to the SiO2 and Al2O3 contents of the rocks, respectively, as well as the secondary structures.Some factors such as the presence of secondary structures, continuous surface area, particle size, and mineralogical composition play an important role in the failure modes of these rocks. UCS and Brazilian strength of schists vary from 10 MPa to 72 MPa and 1.9 to 10.2 MPa, respectively. The lowest UCS occurs in strongly weathered rocks with low silica content. However, the type of clay minerals is effective in the stability of the mineral wall. Considering the presence of montmorillonite clay mineral in the eastern wall of Chahkhatoun mine, the rock resistance is moderate despite the high percentage of silica. UCS values of wet and dry rock samples containing muscovite and montmorillonite clay minerals were more different from those of other rocks. In this regard, the rocks with Illite clay minerals are more resistant than Smectite and montmorillonite minerals. In general, the resistance of schists depends on various factors such as mineralogy, which is of great importance because of its involvement in the formation of secondary structures.



./files/site1/files/%D8%AC%D8%B9%D9%81%D8%B1%DB%8C_%D9%82%D8%B1%DB%8C%D9%87.pdf

Keywords

1. Sonmez, H., Ulusay, R., ”A discussion on Hoek-Brown failure criterion and suggested modification to the criterion verified by slope stability case studies, Yerbilimleri”, Earthscinces, P 26-77, (2002).
2. Sahoo P. R., Venkatesh, A. S.,.”Indicator’ carbonaceous phyllite/graphitic schist in the Archean Kundarkocha gold deposit, Singhbhum orogenic belt, eastern India: Implications for gold mineralization vis-a-vis organic matter”, J. Earth Syst. Sci. 123, No. 7, October 2014, pp. 1693–1703 (2014).
3. Ahn J. H, Moonsup C., Busek P R., “Interstratifications of carbonaceous material within illite; Am. Mineral” 84 1967–1970, (1999).
4. Banerjee A. K., Thiagarajan T A., “Progress report of investigation of gold at Kunderkocha Singhbhum district, Bihar; Bull” Geol. Surv. India Ser. A 38 106, (1965).
5. Bierlein F. P., Cartwright I., McKnight S., “The role of carbonaceous ‘Indicator’ slates in the genesis of lode gold mineralization in the western Lachlan Orogen, Victoria, southeast Australia”; Econ. Geol. 96 431–451, (2001).
6. Craw D., “Geochemistry of late metamorphic hydrothermal alteration and graphitization of host rock, Macraes gold mine, Otago Schist, New Zealand; Chem” Geol. 191 257–275, (2002).
7. Bottrel S. H., Shepherd T. J., Yardley B. W. D., Dubessy J., “A fluid inclusion model for the genesis of the ore of the Dolyellau gold belt, North Wales; J” Journal of the Geological Society London 145 139–145, (1988).
8. Diessel C. F. K., Brothers R. N., Black P. M., “Coalificationand graphitization of high-pressure schists in NewCaledonia; Contrib. Mineral” Petrol. 68 63–78, (1978).
9. Gupta A., “Gold mineralization in the eastern segmentof Indian Precambrian shield: A review; In: Gold Metallogeny, India and beyond (eds)” Deb M and Goldfarb R, pp. 256–280, (2010).
10. Liu, Z., Jianfu, Sh., Xie, Sh., Conil, N., Zha, W., “Effectes of relative humidity and mineral compositions on creep deformation and failure of claystone under compression” International Journal of Rocks Mechanics and Mining Sciences, 103, p 68-76, (2018).
12. Kretzschmar, R., Robarge, W. P., Amoozegar, A., Vepraskas, M,J., “Biotite alteration to hallosite and kaolinite in soil –saprolite profiles developed from mica Schist and granite gneiss”, Geoderma, 75, p. 155-170, (1997).
13. Xiao- ping Zhang, Zh., Louis Ngai Yuen, Y., Wong, Si-Jing Wang, W., Geng-You Han, H., “Engineering properties of quartz mica Scist”, Engineering Geology, 121, p 135-149, (2011).
14. Hemmati A., Ghafoori, M., Moomivand, H., Lashkaripoor Gh. R., “The effect of mineralogy and textural charactrstics on the strenght of crystalline igneous rocks using image-based textural quantification”, Engineeribg geology, 266, 105467, (2020).
15. Ündül, Ö., “ Assessment of mineralogical and petrographic factors affecting petrophysical properties, strength and cracking processes of volcanic rocks”. Engineeribg geology 210, 10–22, (2016).
16. Lan, H., Martin, C. D., Hu, B., “Effect of hetrogeneity of brittle rock on micromechanical extensile behavior during compression loading”, Journal of Geophysical Research: solid Earth, 115 (B1): 1-14, (2010).
17. Jung-woo, Ch. Hanna, K. Seokwon, J. Ki-Bok, M. ., “Deformation and strength anisotropy of Asan gneiss, Boryeong shale, and Yeoncheon schist ”, International Journal of Rock Mechanics & Mining Sciences , 50 -158-169, (2012).