Earth Sciences by I. Dar

By I. Dar

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50 40 30 completely weathered (V) h ighly weathered (IV) residuel moderately weathered (III) 10 s l ightly weathered (II) 20 0 40 60 80 s econd ry minerals content (%) 20 100 crack density+ the ammount of voids increasing Fig. 4. The definition of weathering degree based on mineralogical change and the physical change caused by weathering processes(a) and the secondary mineral content and microfissuring index Ceryan et al. (2008b) said that If Imp and Ifp are shown on the distance axis in the cartesian coordinate system, the distance from the origin will show the weathering condition of the sample.

Engineering geology of Afyon Marbles and the relationships between its physicomechanical properties and weathering. D. Thesis İstanbul Technical. University, Istanbul, Turkey, (in Turkish). Guolin R, Yushan L (1990). Engineering geological zonation of Xiamen granitic weathered crust and bearing capacity of residual soil. 6 th International IAEG Congress, 19891996, Balkema Rotterdam. Gupta. S. S. 2001. Weathering indices and their applicability for crystalline rocks. ,60, 201-221 Gurocak Z, Kilic, R.

Thesis. Karadeniz Technical. University, Trabzon, Turkey, 300p, (in Turkish) Ceryan, Ş. 2008. New Chemical Weathering Indices for Estimating Engineering Properties of Rocks: A Case Study from Kürtün Granodiorite, NE Turkey, Turkish Journal of Earth Sciences, 17, 187-207 Ceryan, Ş. and Ceryan, N. 2005. The relationship between the chemical weathering indices and potential durability of stone in service. , Ceryan N. and Aydın, A. 2005. Determination of Weathering In Engineering Time Using Interaction Matrices.

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