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    ΠœΠΈΠ½Π΅Ρ€Π°Π»ΠΎΠ³ΠΈΡ‡Π΅ΡΠΊΠΈΠ΅ исслСдования Π² ΠΏΠ΅Ρ‰Π΅Ρ€Π½ΠΎΠΉ систСмС БнСТная-МСТСнного-Иллюзия (Π—Π°ΠΏΠ°Π΄Π½Ρ‹ΠΉ Кавказ, Бзыбский Ρ…Ρ€Π΅Π±Π΅Ρ‚): ΠΏΡ€Π΅Π΄Π²Π°Ρ€ΠΈΡ‚Π΅Π»ΡŒΠ½Ρ‹Π΅ Ρ€Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹ ΠΈ направлСния Π΄Π°Π»ΡŒΠ½Π΅ΠΉΡˆΠΈΡ… Ρ€Π°Π±ΠΎΡ‚

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    Π’ ΡΡ‚Π°Ρ‚ΡŒΠ΅ приводятся свСдСния ΠΎ ΠΌΠΈΠ½Π΅Ρ€Π°Π»ΡŒΠ½ΠΎΠΌ составС Π²ΠΎΠ΄Π½Ρ‹Ρ… Ρ…Π΅ΠΌΠΎΠ³Π΅Π½Π½Ρ‹Ρ… ΠΈ Π²ΠΎΠ΄Π½Ρ‹Ρ… мСханичСских ΠΎΡ‚Π»ΠΎΠΆΠ΅Π½ΠΈΠΉ Π² ΠΏΠ΅Ρ‰Π΅Ρ€Π½ΠΎΠΉ систСмС БнСТная-МСТСнного-Иллюзия. Π’ состав Π²ΠΎΠ΄Π½Ρ‹Ρ… Ρ…Π΅ΠΌΠΎΠ³Π΅Π½Π½Ρ‹Ρ… ΠΎΡ‚Π»ΠΎΠΆΠ΅Π½ΠΈΠΉ входят Mg- ΠΈ Sr-содСрТащий ΠΊΠ°Π»ΡŒΡ†ΠΈΡ‚, Π°Ρ€Π°Π³ΠΎΠ½ΠΈΡ‚, гипс, Π³ΠΈΠ΄Ρ€ΠΎΠΌΠ°Π³Π½Π΅Π·ΠΈΡ‚, цСлСстин, стронцианит, Π΄ΠΎΠ»ΠΎΠΌΠΈΡ‚, Π³Π΅Ρ‚ΠΈΡ‚, Ρ€ΡƒΡ‚ΠΈΠ» ΠΈ Ρ†ΠΈΡ€ΠΊΠΎΠ½. Π’ΠΎΠ΄Π½Ρ‹Π΅ мСханичСскиС отлоТСния слоТСны прСимущСствСнно Π΄ΠΎΠ»ΠΎΠΌΠΈΡ‚ΠΎΠΌ, ΠΊΠ²Π°Ρ€Ρ†Π΅ΠΌ ΠΈ ΠΊΠ°Π»ΡŒΡ†ΠΈΡ‚ΠΎΠΌ. Π’ схоТих ΠΏΠΎ ΠΌΠΎΡ€Ρ„ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ ΠΌΠΈΠΊΡ€ΠΎΠΊΠ»ΠΈΠΌΠ°Ρ‚Ρƒ частях ΠΏΠ΅Ρ‰Π΅Ρ€Π½ΠΎΠΉ систСмы Π½Π°Π±Π»ΡŽΠ΄Π°ΡŽΡ‚ΡΡ ΠΎΠ΄ΠΈΠ½Π°ΠΊΠΎΠ²Ρ‹Π΅ Π²Ρ‚ΠΎΡ€ΠΈΡ‡Π½Ρ‹Π΅ ΠΌΠΈΠ½Π΅Ρ€Π°Π»Ρ‹.Π£ статті Π½Π°Π²ΠΎΠ΄ΡΡ‚ΡŒΡΡ відомості ΠΏΡ€ΠΎ ΠΌΡ–Π½Π΅Ρ€Π°Π»ΡŒΠ½ΠΈΠΉ склад Π²ΠΎΠ΄Π½ΠΈΡ… Ρ…Π΅ΠΌΠΎΠ³Π΅Π½Π½ΠΈΡ… Ρ– Π²ΠΎΠ΄Π½ΠΈΡ… ΠΌΠ΅Ρ…Π°Π½Ρ–Ρ‡Π½ΠΈΡ… Π²Ρ–Π΄ΠΊΠ»Π°Π΄Π΅Π½ΡŒ Π² ΠΏΠ΅Ρ‡Π΅Ρ€Π½Ρ–ΠΉ систСмі Π‘Π½Ρ–ΠΆΠ½Π°-МСТСного-Π†Π»ΡŽΠ·Ρ–Ρ. Π”ΠΎ складу Π²ΠΎΠ΄Π½ΠΈΡ… Ρ…Π΅ΠΌΠΎΠ³Π΅Π½Π½ΠΈΡ… Π²Ρ–Π΄ΠΊΠ»Π°Π΄Π΅Π½ΡŒ Π²Ρ…ΠΎΠ΄ΡΡ‚ΡŒ ΠΊΠ°Π»ΡŒΡ†ΠΈΡ‚, який ΠΌΡ–ΡΡ‚ΠΈΡ‚ΡŒ Mg Ρ– Sr, Π°Ρ€Π°Π³ΠΎΠ½Ρ–Ρ‚, гіпс, Π³Ρ–Π΄Ρ€ΠΎΠΌΠ°Π³Π½Π΅Π·Ρ–Ρ‚, цСлСстин, стронціаніт, Π΄ΠΎΠ»ΠΎΠΌΡ–Ρ‚, Π³Π΅Ρ‚ΠΈΡ‚, Ρ€ΡƒΡ‚ΠΈΠ» Ρ– Ρ†ΠΈΡ€ΠΊΠΎΠ½. Π’ΠΎΠ΄Π½Ρ– ΠΌΠ΅Ρ…Π°Π½Ρ–Ρ‡Π½Ρ– відкладСння складСні ΠΏΠ΅Ρ€Π΅Π²Π°ΠΆΠ½ΠΎ Π΄ΠΎΠ»ΠΎΠΌΡ–Ρ‚ΠΎΠΌ, ΠΊΠ²Π°Ρ€Ρ†ΠΎΠΌ Ρ– ΠΊΠ°Π»ΡŒΡ†ΠΈΡ‚ΠΎΠΌ. Π£ схоТих Π·Π° ΠΌΠΎΡ€Ρ„ΠΎΠ»ΠΎΠ³Ρ”ΡŽ Ρ‚Π° ΠΌΡ–ΠΊΡ€ΠΎΠΊΠ»Ρ–ΠΌΠ°Ρ‚ΠΎΠΌ частинах ΠΏΠ΅Ρ‡Π΅Ρ€Π½ΠΎΡ— систСми ΡΠΏΠΎΡΡ‚Π΅Ρ€Ρ–Π³Π°ΡŽΡ‚ΡŒΡΡ ΠΎΠ΄Π½Π°ΠΊΠΎΠ²Ρ– Π²Ρ‚ΠΎΡ€ΠΈΠ½Π½Ρ– ΠΌΡ–Π½Π΅Ρ€Π°Π»ΠΈ.The article presents the preliminary characteristic of the mineral composition of chemogenic formations and clastic deposits of Snezhnaya-Mezhennogo-Illusia cave system. Chemogenic formations are composed by Mg- and Sr-calcite, aragonite, gypsum and hydromagnesite, celestite, strontianite, dolomite, goethite, rutile and zircon. Clastic sediments are composed mainly by dolomite, quartz and calcite. Same secondary minerals are observed in those parts of the cave system that have similar morphology and microclimate

    Vaginal prolapse repair with or without a midurethral sling in women with genital prolapse and occult stress urinary incontinence: a randomized trial

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    We compared pelvic organ prolapse (POP) repair with and without midurethral sling (MUS) in women with occult stress urinary incontinence (SUI). This was a randomized trial conducted by a consortium of 13 teaching hospitals assessing a parallel cohort of continent women with symptomatic stage II or greater POP. Women with occult SUI were randomly assigned to vaginal prolapse repair with or without MUS. Women without occult SUI received POP surgery. Main outcomes were the absence of SUI at the 12-month follow-up based on the Urogenital Distress Inventory and the need for additional treatment for SUI. We evaluated 231 women, of whom 91 randomized as follows: 43 to POP surgery with and 47 without MUS. A greater number of women in the MUS group reported absence of SUI [86 % vs. 48 %; relative risk (RR) 1.79; 95 % confidence interval (CI) 1.29-2.48]. No women in the MUS group received additional treatment for postoperative SUI; six (13 %) in the control group had a secondary MUS. Women with occult SUI reported more urinary symptoms after POP surgery and more often underwent treatment for postoperative SUI than women without occult SUI. Women with occult SUI had a higher risk of reporting SUI after POP surgery compared with women without occult SUI. Adding a MUS to POP surgery reduced the risk of postoperative SUI and the need for its treatment in women with occult SUI. Of women with occult SUI undergoing POP-only surgery, 13 % needed additional MUS. We found no differences in global impression of improvement and quality of lif
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