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    ΠœΠΎΡ€Ρ„ΠΎΠ»ΠΎΠ³ΠΈΡ, строСниС ΠΈ состав Ρ†ΠΈΡ€ΠΊΠΎΠ½Π° ΠΈΠ· мСтапСсчаников алькСсвоТской Ρ‚ΠΎΠ»Ρ‰ΠΈ (ΠŸΡ€ΠΈΠΏΠΎΠ»ΡΡ€Π½Ρ‹ΠΉ Π£Ρ€Π°Π»)

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    Description of the features of morphology, internal structure, and analysis results of Th/U and Zr/Hf ratios in zircons from sandstones of the gold-bearing Alkesvozhskaya sequence, located at the basement of the Paleozoic section in the Subpolar Urals, is presented. It has been established that most of the studied zircons are primary igneous grains of the first weathering cycle. The detrital zircon source was probably in formations close in age, underlying or located nearby felsic and basic volcanics of igneous complexes of different stages of formation of Timanides-protouralides, associated granitoids, and intrusive mafic formations. Small part of well-rounded zircon Pre-Riphean grains can be redeposited from the Riphean metasedimentary formations, which, in turn, inherited it from the rocks of the ancient basement of the East European PlatformΠŸΡ€ΠΈΠ²Π΅Π΄Π΅Π½Ρ‹ описаниС особСнностСй ΠΌΠΎΡ€Ρ„ΠΎΠ»ΠΎΠ³ΠΈΠΈ, Π²Π½ΡƒΡ‚Ρ€Π΅Π½Π½Π΅Π³ΠΎ строСния ΠΈ Π°Π½Π°Π»ΠΈΠ· ΠΎΡ‚Π½ΠΎΡˆΠ΅Π½ΠΈΠΉ Th/U ΠΈ Zr/Hf Π² Ρ†ΠΈΡ€ΠΊΠΎΠ½Π°Ρ… ΠΈΠ· пСсчаников золотоносной алькСсвоТской Ρ‚ΠΎΠ»Ρ‰ΠΈ, располоТСнной Π² основании палСозойского Ρ€Π°Π·Ρ€Π΅Π·Π° Π½Π° ΠŸΡ€ΠΈΠΏΠΎΠ»ΡΡ€Π½ΠΎΠΌ Π£Ρ€Π°Π»Π΅. УстановлСно, Ρ‡Ρ‚ΠΎ Π±ΠΎΠ»ΡŒΡˆΠΈΠ½ΡΡ‚Π²ΠΎ ΠΈΠ·ΡƒΡ‡Π΅Π½Π½Ρ‹Ρ… Ρ†ΠΈΡ€ΠΊΠΎΠ½ΠΎΠ² ΡΠ²Π»ΡΡŽΡ‚ΡΡ ΠΏΠ΅Ρ€Π²ΠΈΡ‡Π½ΠΎ-магматичСскими Π·Π΅Ρ€Π½Π°ΠΌΠΈ ΠΏΠ΅Ρ€Π²ΠΎΠ³ΠΎ Ρ†ΠΈΠΊΠ»Π° вывСтривания. Π˜ΡΡ‚ΠΎΡ‡Π½ΠΈΠΊΠΎΠΌ ΠΎΠ±Π»ΠΎΠΌΠΎΡ‡Π½ΠΎΠ³ΠΎ Ρ†ΠΈΡ€ΠΊΠΎΠ½Π°, вСроятно, являлись Π±Π»ΠΈΠ·ΠΊΠΈΠ΅ ΠΏΠΎ Π²Ρ€Π΅ΠΌΠ΅Π½ΠΈ образования ΠΏΠΎΠ΄ΡΡ‚ΠΈΠ»Π°ΡŽΡ‰ΠΈΠ΅ ΠΈΠ»ΠΈ располоТСнныС поблизости кислыС ΠΈ основныС Π²ΡƒΠ»ΠΊΠ°Π½ΠΈΡ‚Ρ‹ магматичСских комплСксов Ρ€Π°Π·Π»ΠΈΡ‡Π½Ρ‹Ρ… стадий формирования Ρ‚ΠΈΠΌΠ°Π½ΠΈΠ΄-ΠΏΡ€ΠΎΡ‚ΠΎΡƒΡ€Π°Π»ΠΈΠ΄, Π°ΡΡΠΎΡ†ΠΈΠΈΡ€ΡƒΡŽΡ‰ΠΈΠ΅ с Π½ΠΈΠΌΠΈ Π³Ρ€Π°Π½ΠΈΡ‚ΠΎΠΈΠ΄Ρ‹ ΠΈ ΠΈΠ½Ρ‚ΡƒΠ·ΠΈΠ²Π½Ρ‹Π΅ образования основного состава. ΠΠ΅Π·Π½Π°Ρ‡ΠΈΡ‚Π΅Π»ΡŒΠ½Π°Ρ Ρ‡Π°ΡΡ‚ΡŒ Ρ…ΠΎΡ€ΠΎΡˆΠΎ ΠΎΠΊΠ°Ρ‚Π°Π½Π½Ρ‹Ρ… Π·Π΅Ρ€Π΅Π½ Ρ†ΠΈΡ€ΠΊΠΎΠ½Π° с дорифСйскими Π΄Π°Ρ‚ΠΈΡ€ΠΎΠ²ΠΊΠ°ΠΌΠΈ ΠΌΠΎΠΆΠ΅Ρ‚ Π±Ρ‹Ρ‚ΡŒ ΠΏΠ΅Ρ€Π΅ΠΎΡ‚Π»ΠΎΠΆΠ΅Π½Π° ΠΈΠ· рифСских мСтаосадочных ΠΎΠ±Ρ€Π°Π·ΠΎΠ²Π°Π½ΠΈΠΉ, Π² свою ΠΎΡ‡Π΅Ρ€Π΅Π΄ΡŒ ΡƒΠ½Π°ΡΠ»Π΅Π΄ΠΎΠ²Π°Π²ΡˆΠΈΡ… Π΅Π³ΠΎ ΠΈΠ· ΠΏΠΎΡ€ΠΎΠ΄ Π΄Ρ€Π΅Π²Π½Π΅Π³ΠΎ Ρ„ΡƒΠ½Π΄Π°ΠΌΠ΅Π½Ρ‚Π° Восточно-ЕвропСйской ΠΏΠ»Π°Ρ‚Ρ„ΠΎΡ€ΠΌΡ‹

    Rhabdomyolisys as a Cause of Acute Renal Injury

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    Rhabdomyolysis (RM) is defined as striate muscle-cell damage with disintegration of skeletal muscles and release of intracellular constituents to the circulation, with or without subsequent kidney injury. RM is one of the leading causes of acute kidney injury and is associated with substantial morbidity. The major signs of acute kidney injury in rhabdomyolysis are: pain, weakness and swelling of the injured muscle or muscle groups and myoglobinuria with reddish discoloration of the urine and decrease in urine output to anuria. The authors describe three cases of rhabdomyolysis with acute renal injury and discuss the current knowledge on the etiopathogenesis, clinical manifestations, diagnosis and treatment of this condition
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