11 research outputs found

    Modern Techniques for Cervical Cancer Radiotherapy

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    Cervical cancer is a socially significant illness often impacting women of reproductive and working age. The patients’ young age and social activity warrant the development of effective and safe therapies.The past decades have witnessed the novel radiation techniques to contain cervical cancer: 3DCRT-3D, IMRT, and VMAT, adaptive radiotherapy, CT/MRI-guided intracavitary radiation, combined interstitial and intracavitary radiation, abandoning intracavitary intervention for external beam delivery with sequential or concurrent cervical dose escalation, under brachytherapy unfeasible.Modern equipment and treatment planning systems allow a high dose delivery to the tumour and intracavitary treatment with visual control of the target and organs at risk. Combining of intracavitary and interstitial radiotherapy enables a better dose coverage of the target at a minimal radiation impact on organs at risk.Phasing-out of intracavitary for external radiotherapy may enable a cancericide dose delivery to the tumour under intractable intracavitary treatment.The major goal of technic novelties is the establishment of personalised radiotherapy for improving treatment outcomes and reducing the incidence and/or severity of radiation side effects. The article overviews the radiotherapy techniques for cervical cancer treatment and routes of their development

    Π‘ΠΎΠ²Ρ€Π΅ΠΌΠ΅Π½Π½Ρ‹Π΅ ΠΌΠ΅Ρ‚ΠΎΠ΄Ρ‹ Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ Ρ€Π°ΠΊΠ° шСйки ΠΌΠ°Ρ‚ΠΊΠΈ

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    Cervical cancer is a socially significant illness often impacting women of reproductive and working age. The patients’ young age and social activity warrant the development of effective and safe therapies.The past decades have witnessed the novel radiation techniques to contain cervical cancer: 3DCRT-3D, IMRT, and VMAT, adaptive radiotherapy, CT/MRI-guided intracavitary radiation, combined interstitial and intracavitary radiation, abandoning intracavitary intervention for external beam delivery with sequential or concurrent cervical dose escalation, under brachytherapy unfeasible.Modern equipment and treatment planning systems allow a high dose delivery to the tumour and intracavitary treatment with visual control of the target and organs at risk. Combining of intracavitary and interstitial radiotherapy enables a better dose coverage of the target at a minimal radiation impact on organs at risk.Phasing-out of intracavitary for external radiotherapy may enable a cancericide dose delivery to the tumour under intractable intracavitary treatment.The major goal of technic novelties is the establishment of personalised radiotherapy for improving treatment outcomes and reducing the incidence and/or severity of radiation side effects. The article overviews the radiotherapy techniques for cervical cancer treatment and routes of their development.Π Π°ΠΊ шСйки ΠΌΠ°Ρ‚ΠΊΠΈ являСтся ΡΠΎΡ†ΠΈΠ°Π»ΡŒΠ½ΠΎ Π·Π½Π°Ρ‡ΠΈΠΌΡ‹ΠΌ Π·Π°Π±ΠΎΠ»Π΅Π²Π°Π½ΠΈΠ΅ΠΌ ΠΈ часто диагностируСтся Ρƒ ΠΆΠ΅Π½Ρ‰ΠΈΠ½ Ρ€Π΅ΠΏΡ€ΠΎΠ΄ΡƒΠΊΡ‚ΠΈΠ²Π½ΠΎΠ³ΠΎ ΠΈ работоспособного возраста. Молодой ΠΈ ΡΠΎΡ†ΠΈΠ°Π»ΡŒΠ½ΠΎ Π°ΠΊΡ‚ΠΈΠ²Π½Ρ‹ΠΉ возраст Π΄Π°Π½Π½Ρ‹Ρ… ΠΏΠ°Ρ†ΠΈΠ΅Π½Ρ‚ΠΎΠ² Π΄Π΅Π»Π°Π΅Ρ‚ Π½Π΅ΠΎΠ±Ρ…ΠΎΠ΄ΠΈΠΌΡ‹ΠΌ Ρ€Π°Π·Ρ€Π°Π±ΠΎΡ‚ΠΊΡƒ эффСктивных ΠΈ бСзопасных ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠ² лСчСния.Π—Π° послСдниС дСсятилСтия появились Π½ΠΎΠ²Ρ‹Π΅ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠΈ Π»ΡƒΡ‡Π΅Π²ΠΎΠ³ΠΎ лСчСния Ρ€Π°ΠΊΠ° шСйки ΠΌΠ°Ρ‚ΠΊΠΈ: Π²Π½Π΅Π΄Ρ€Π΅Π½ΠΈΠ΅ 3DCRT-3D, IMRT ΠΈ VMAT, адаптивная лучСвая тСрапия, ΠΏΠ»Π°Π½ΠΈΡ€ΠΎΠ²Π°Π½ΠΈΠ΅ внутриполостного облучСния ΠΏΠΎ КВ/МРВ-изобраТСниям, ΠΊΠΎΠΌΠ±ΠΈΠ½ΠΈΡ€ΠΎΠ²Π°Π½ΠΈΠ΅ Π²Π½ΡƒΡ‚Ρ€ΠΈΡ‚ΠΊΠ°Π½Π΅Π²ΠΎΠΉ ΠΈ внутриполостной Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ, Π·Π°ΠΌΠ΅Π½Π° внутриполостного этапа Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ дистанционным ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½Ρ‚ΠΎΠΌ с ΠΏΠΎΡΠ»Π΅Π΄ΠΎΠ²Π°Ρ‚Π΅Π»ΡŒΠ½ΠΎΠΉ ΠΈΠ»ΠΈ ΠΎΠ΄Π½ΠΎΠ²Ρ€Π΅ΠΌΠ΅Π½Π½ΠΎΠΉ эскалациСй Π΄ΠΎΠ·Ρ‹ Π½Π° ΡˆΠ΅ΠΉΠΊΡƒ ΠΌΠ°Ρ‚ΠΊΠΈ ΠΏΡ€ΠΈ нСвозмоТности провСдСния Π±Ρ€Π°Ρ…ΠΈΡ‚Π΅Ρ€Π°ΠΏΠΈΠΈ.Π‘ΠΎΠ²Ρ€Π΅ΠΌΠ΅Π½Π½ΠΎΠ΅ ΠΎΠ±ΠΎΡ€ΡƒΠ΄ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΈ систСмы планирования ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡŽΡ‚ ΠΏΠΎΠ΄Π²ΠΎΠ΄ΠΈΡ‚ΡŒ высокиС Π΄ΠΎΠ·Ρ‹ Π½Π° ΠΎΠΏΡƒΡ…ΠΎΠ»ΡŒ, ΠΏΡ€ΠΎΠ²ΠΎΠ΄ΠΈΡ‚ΡŒ Π²Π½ΡƒΡ‚Ρ€ΠΈΠΏΠΎΠ»ΠΎΡΡ‚Π½ΡƒΡŽ Π»ΡƒΡ‡Π΅Π²ΡƒΡŽ Ρ‚Π΅Ρ€Π°ΠΏΠΈΡŽ ΠΏΠΎΠ΄ Π²ΠΈΠ·ΡƒΠ°Π»ΡŒΠ½Ρ‹ΠΌ ΠΊΠΎΠ½Ρ‚Ρ€ΠΎΠ»Π΅ΠΌ мишСни ΠΈ ΠΎΡ€Π³Π°Π½ΠΎΠ² риска. ΠšΠΎΠΌΠ±ΠΈΠ½Π°Ρ†ΠΈΡ внутриполостной ΠΈ Π²Π½ΡƒΡ‚Ρ€ΠΈΡ‚ΠΊΠ°Π½Π΅Π²ΠΎΠΉ Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ Π΄Π°Π΅Ρ‚ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡ‚ΡŒ Π»ΡƒΡ‡ΡˆΠ΅Π³ΠΎ ΠΎΡ…Π²Π°Ρ‚Π° мишСни Π΄ΠΎΠ·ΠΎΠΉ, максимально ΠΈΡΠΊΠ»ΡŽΡ‡Π°Ρ ΠΎΡ€Π³Π°Π½Ρ‹ риска ΠΈΠ· Π·ΠΎΠ½Ρ‹ облучСния.Π—Π°ΠΌΠ΅Π½Π° внутриполостного этапа Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ дистанционным ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½Ρ‚ΠΎΠΌ ΠΌΠΎΠΆΠ΅Ρ‚ Π΄Π°Ρ‚ΡŒ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡ‚ΡŒ подвСсти ΠΊΠ°Π½Ρ†Π΅Ρ€ΠΈΡ†ΠΈΠ΄Π½ΡƒΡŽ Π΄ΠΎΠ·Ρƒ ΠΊ ΠΎΠΏΡƒΡ…ΠΎΠ»ΠΈ ΠΏΡ€ΠΈ нСвозмоТности провСдСния внутриполостного лСчСния.ЦСлью поиска ΠΈ внСдрСния Π½ΠΎΠ²Ρ‹Ρ… ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊ являСтся пСрсонифицированная оптимизация Π»ΡƒΡ‡Π΅Π²ΠΎΠΉ Ρ‚Π΅Ρ€Π°ΠΏΠΈΠΈ для ΡƒΠ»ΡƒΡ‡ΡˆΠ΅Π½ΠΈΡ Ρ€Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚ΠΎΠ² лСчСния, сниТСния частоты ΠΈ/ΠΈΠ»ΠΈ выраТСнности ΠΏΠΎΠ±ΠΎΡ‡Π½Ρ‹Ρ… эффСктов Ρ€Π°Π΄ΠΈΠΎΡ‚Π΅Ρ€Π°ΠΏΠΈΠΈ. Π’ Π΄Π°Π½Π½ΠΎΠΉ ΡΡ‚Π°Ρ‚ΡŒΠ΅ прСдставлСн ΠΎΠ±Π·ΠΎΡ€ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠ² Π»ΡƒΡ‡Π΅Π²ΠΎΠ³ΠΎ лСчСния Ρ€Π°ΠΊΠ° шСйки ΠΌΠ°Ρ‚ΠΊΠΈ ΠΈ Π½Π°ΠΏΡ€Π°Π²Π»Π΅Π½ΠΈΠΉ ΠΈΡ… развития

    U/Pb Age of detrital zircons from sandstones of the upper emsian diamond takaty formation of the Western Urals

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    The first results of U/Pb (LA-ICP-MS) dating of detrital zircons from quartz sandstones of the Devonian Takaty Formation are presented. The obtained ages span a range from 1857.5 Β± 53.8 to 3054.0 Β± Β± 48.0 Ma. The vast Β«gapΒ» (~1.5 Ga) between sedimentary age of Takaty Formation and the age of the youngest zircon grain is fixed. A comparison of known ages of crystalline complexes from the Volga-Uralian part of East-European Platform with obtained ages of detrital zircons from Takaty Formation supports the Β«Volgo-UralianΒ» origin of the zircons. This implies the existence of a previously unknown stage of kimberlitic magmatism, much more ancient than the stage of kimberlitic magmatism formed diamonds in Arkhangelsk and Timan provinces

    First results of U-Pb dating of detrital zircons from the Upper Ordovician sandstones of the Bashkir uplift (Southern Urals)

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    The first results of U–Pb dating of detrital zircons from Upper Ordovician sandstones of the Bashkir uplift in the Southern Urals and U–Pb isotopic ages available for detrital zircons from six stratigraphic levels of the Riphean–Paleozoic section of this region are discussed. It is established that the long (approximately 1.5 Ga) depositional history of sedimentary sequences of the Bashkir uplift includes a peculiar period lasting from the Late Vendian to the Emsian Age of the Early Devonian (0.55–0.41 Ga). This period is characterized by the following features: (1) prevalence of material from eroded Mesoproterozoic and Early Neoproterozoic crystalline complexes among clastics with ages atypical of the Volga–Urals segment of the East European Platform basement; (2) similarity of age spectra obtained for detrital zircons from different rocks of the period: Upper Vendian–Lower Cambrian lithic sandstones and Middle Ordovician substantially quartzose sandstones.6 page(s

    Some general features of the Western Urals terrigenous deposits formation: Synthesis of U-Pb isotopic age data of detrital zircon and geochemical investigation of the sales and mudstones

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    The data on U-Pb-isotopic ages of detrital zircons from Riphean-Paleozoic and Early Triassic sandstones and geochemistry of shales and mudstones of the Western Urals are discussed. The ages of detrital zircons suggest that the sand material for sedimentary basins existed at the junction of the East European Platform and Urals during more than one and a half billion years, has been brought mainly from the platform. Tectonogenic sands (according F.J. Pettijohn and co-authors) as a part of the Western Urals sedimentary associations play a significant role only in Vendian and in the last third of the Paleozoic. During the rest of the time was dominated cratonogenic sands. According to clay rocks geochemical characteristics during the time from 1750 to 250 Ma, there are unidirectional trend in the composition of the erosion areas: increasing mafic and ultramafic igneous rocks which reached to maximum in Early Permian time
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