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ПЕРЕКРЕСТНОЕ СУБСИДИРОВАНИЕ КАК ИНСТРУМЕНТ ФОРМИРОВАНИЯ ТАРИФОВ СЕТЕВЫХ КОМПАНИЙ: ОПРАВДАНА ЛИ ОТМЕНАPositive and negative aspects of cross-subsidization are considered and it is concluded

Влияние тарифной политики и системы перекрестного субсидирования на экономическую эффективность оборудования, преобразовывающего электрическую энергию в тепловуюInfluence of tariff policy and cross-subsiding system on the economic efficiency of equipment

Subsidized Loan Financing and its Impact on the Cost of Capital and Levered Firm ValueSubsidized Loan Financing and its Impact on the Cost of Capital and Levered Firm Value

InSAR Applications of Land Subsidence Over Oil Fields (Case Study Southeast of Republic of Tatarstan, Russia)Land subsidence risk assessment basically based on current information found that the analyzed

Development of consumers’ behavior business model on energy market in the energy markets are changing to address the problems of cross-subsidization. The introduction of new

SOFTWARE DEVELOPMENT FOR OPTIMIZATION OF THE RANGE OF SUBSIDIZED MEDICINESFOR THE TREATMENT OF PATIENTS WITH DIABETES
SOFTWARE DEVELOPMENT FOR OPTIMIZATION OF THE RANGE OF SUBSIDIZED MEDICINESFOR THE TREATMENT

Geodesic investigation of land surface crack dynamics in the zone of land subsidence with loamy soils in central IranGeodesic investigation of land surface crack dynamics in the zone of land subsidence with loamy

Subcidence patterns (rate of evolution) of Moscow basinMoscow basin had subsided in two “half-waves” velocity regime over the time-span: Cambrian (Vendian

Outcrop analogue study of Permocarboniferous geothermal sandstone reservoir formations (northern Upper Rhine Graben, Germany): impact of mineral content, depositional environment and diagenesis on petrophysical properties investigated in large-scale studies only. The Cenozoic Upper Rhine Graben crosses the Permocarboniferous Saar

Outcrop analogue study of Permocarboniferous geothermal sandstone reservoir formations (northern Upper Rhine Graben, Germany): impact of mineral content, depositional environment and diagenesis on petrophysical properties investigated in large-scale studies only. The Cenozoic Upper Rhine Graben crosses the Permocarboniferous Saar

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