Acknowledgement
This paper is funded by the Government of the Republic of Serbia (The Science Fund of the Republic of Serbia), as a part of Serbian Science and Diaspora Collaboration Program - project Rock slope stability - back analysis of failures along rock cuttings - ROCKSTAB (application number 6524757). Also, the Erasmus+ grant (EMADRID03) for the stay of Professor Svetlana Melentijevic at the University of Belgrade is acknowledged.
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