journal of mining institute سال:2024 - دوره:266

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journal of mining institute
سال:2024 - دوره:266 - شماره:0

assessment of rock massif sustainability in the area of the underground research laboratory (nizhnekanskii massif, enisei site) - صفحه:167-178 assessment of the contribution of precambrian deposits in forming the petroleum potential of the eastern part of the volga-urals basin using results of modeling - صفحه:199-217 comprehensive assessment of deformation of rigid reinforcing system during convergence of mine shaft lining in unstable rocks - صفحه:305-315 depth distribution of radiation defects in irradiated diamonds by confocal raman spectroscopy - صفحه:179-187 directions in the technological development of aluminium pots - صفحه:246-259 justification of the approaches to improve management strategy of the mining system based on the analysis of data on the mining of complex structural rock blocks - صفحه:316-325 localization of sites for the development of geomechanical processes in underground workings based on the results of the transformation and classification analysis of seismic data - صفحه:260-271 microstructural features of chromitites and ultramafic rocks of the almaz-zhemchuzhina deposit (kempirsai massif, kazakhstan) according to electron backscatter diffraction (ebsd) studies - صفحه:218-230 modeling the efficiency of seasonal cooling devices when changing the statistical distribution of weather conditions - صفحه:272-282 optimization of specific energy consumption for rock crushing by explosion at deposits with complex geological structure - صفحه:231-245 predictive assessment of ore dilution in mining thin steeply dipping deposits by a system of sublevel drifts - صفحه:283-294 study on the thin layer drying and diffusion mechanism of low rank coal in inner mongolia and yunnan - صفحه:326-338 technology of absorption elimination with cross-linking plugging material based on cement and cross-linked polymer - صفحه:295-304 velocity structure of the earth’s crust and upper mantle in the pechenga ore region and adjacent areas in the northwestern part of the lapland-kola orogen by the receiver function technique - صفحه:188-198