Архив научных статейиз журнала «Геоморфология»
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ИРРИГАЦИОННАЯ ГЕОТЕХНОМОРФОСИСТЕМА (КОММЕНТАРИЙ РЕЦЕНЗЕНТА)
РОЗАНОВ Л.Л. — 2009 г.
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ИРРИГАЦИОННЫЙ РЕЛЬЕФ И ФАКТОРЫ, ОПРЕДЕЛЯЮЩИЕ ЕГО УСТОЙЧИВОСТЬ
ИВАНОВ Н.Н. — 2009 г.
The low stability of man-made irrigated relief in the southern regions of Russia produces the unfavorable ecological situation there. One of the main problems at reconstruction and designing of irrigation systems is the evaluation of the main relief stability factors: relief-forming rocks, technogenic sediments, morphology of initial and irrigation relief. The most instability is incidental to relief of check plots on mantle loam.
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ИССЛЕДОВАНИЯ АККУМУЛЯЦИИ НАНОСОВ НА РЕЧНЫХ ПОЙМАХ: МЕТОДИЧЕСКИЕ ВОЗМОЖНОСТИ И ПЕРСПЕКТИВЫ
ГОЛОСОВ В.Н. — 2009 г.
A wide set of methods may be applied for detailed spatial-temporal analysis of floodplain formation within different parts of river valley. Some results of various methods use for the assessment of deposition rates on the floodplain are presented. Perspectives of floodplain deposition rates application for the fundamental and applied investigations are described.
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КОТЛОВИНЫ ОЗЕР КРАСНОЕ И ДАНИЛИЩЕ В МОСКОВСКОЙ ОБЛАСТИ: РЕЛИКТОВЫЕ КРИОГЕННЫЕ ФОРМЫ ИЛИ МЕТЕОРИТНЫЕ КРАТЕРЫ?
БРОНГУЛЕЕВ В.ВАД., ЖИДКОВ М.П., МАКАРЕНКО А.Г. — 2009 г.
The crater-like basins of the lakes Krasnoye and Danilische in the Moscow region are very peculiar and rare forms in the Central Russia. The lakes are stagnant pools up to 10 m deep and 300-400 m in diameter surrounded by annular bank 3-5 m height (9 m at maximum). The shape of the basins allows two hypotheses of their origin: 1 - the impact structures, likewise the basin of the lake Smerdyach'e 50 km apart, which is considered to be astrobleme of 10-25 m y age [3], 2 - destructed pingos of Late Valdai periglacial epoch. The further investigation of the bank section, its age and composition is needed to validate one of these hypotheses.
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ЛАНДШАФТНО-ГЕОМОРФОЛОГИЧЕСКИЙ АНАЛИЗ КАК ОСНОВА РАЗВИТИЯ ЭКОЛОГИЧЕСКОГО ТУРИЗМА НА ЛОКАЛЬНОЙ ТЕРРИТОРИИ (НА ПРИМЕРЕ ВОРОТЫНСКОГО ЗАВОЛЖЬЯ)
АСТАШИН А.Е., ФРИДМАН Б.И. — 2009 г.
Geomorphological and landscape characteristics of Vorotynskoie Zavolzhie were studied. Four landscapes were distinguished within this territory, and optimal approach to tourism planning was outlined.
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ЛИТОГЕННЫЕ СТУПЕНИ ВЫРАВНИВАНИЯ
УФИМЦЕВ Г.Ф. — 2009 г.
A special type of local plantain surfaces is described - lithogenic steps, subhorizontal or slightly tilted, worked along the bedding. Such steps may arise on the valley flanges, on the slopes or on the summits. They may form stepped slope complexes morphologically similar to piedmont steps.
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МЕЖДУНАРОДНЫЙ СИМПОЗИУМ ПО ИЗУЧЕНИЮ ПЕЩЕРНЫХ ЛЬДОВ - IWIC-III
ТРОФИМОВА Е.В. — 2009 г.
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МЕТОДИКА СОСТАВЛЕНИЯ КАРТЫ ЭНЕРГИИ РЕЛЬЕФА
МЕХБАЛИЕВ М.М. — 2009 г.
Actual methods of relief energy maps compilation are discussed, and a new one is proposed. This method counts the potential energy and morphometric characteristics of slopes: area, average angle, density and depth of dissection, exposure, average height.
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МОРФОМЕТРИЧЕСКИЙ АНАЛИЗ РЕЛЬЕФА С ИСПОЛЬЗОВАНИЕМ ГИС-ТЕХНОЛОГИЙ ПРИ ОЦЕНКЕ РЕКРЕАЦИОННОГО ПОТЕНЦИАЛА ЛАГОНАКСКОГО НАГОРЬЯ (СЕВЕРО-ЗАПАДНЫЙ КАВКАЗ)
АНТИПЦЕВА Ю.О., ДУМИТ Ж.А. — 2009 г.
The new methods of morphometric maps compilation with the use of GIS-technologies were developed. Such maps were compiled for the territory of Lagonak highland and were used for the assessment of its recreational potential.
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МОРФОСТРУКТУРНЫЕ И МОРФОСКУЛЬПТУРНЫЕ ОСОБЕННОСТИ РЕЛЬЕФА, РАЗВИТОГО НА ВУЛКАНИЧЕСКИХ ПОРОДАХ НА ГЛАВНОМ ХРЕБТЕ СЕВЕРО-ЗАПАДНОГО КАВКАЗА
НИКОЛАЙЧУК А.В. — 2009 г.
The set of morphostructural blocks of 5th and 6th orders and their limitative faults were determined within the Main Ridge of the North-West Caucasus. The landforms on the volcanic rocks are widespread in the region; by the most part they dominate in relief. Fluvial, nival, and gravitational morphosculptures are predominant.
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НЕКОТОРЫЕ ВОПРОСЫ МЕТОДОЛОГИИ И МЕТОДИКИ МОРФОСТРУКТУРНО-МЕТАЛЛОГЕНИЧЕСКИХ ИССЛЕДОВАНИЙ (ЮГ ДАЛЬНЕГО ВОСТОКА)
ГАВРИЛОВ А.А. — 2009 г.
The effectiveness of morphostructural-metallogenic studies depends in many respect on possibility of: a - revealing the determinate connections between morphotectonic processes and mineralization; b - distinguishing the main types of ore control structures and morphostructures; c - reconstruction of morphostructural pattern of mineralization epochs and analysis of its later transformations. The long-term and multifactor process of Sikhote-Alin orogeny requires the analysis of conformal relations between the structures of different ages, day surface and deep heterogeneity, taking into account the possibility of convergent landforms origin (over-plum depression or collapsed paleoarch).
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НЕКОТОРЫЕ ОСОБЕННОСТИ РАЗВИТИЯ СТУПЕНЧАТЫХ СКЛОНОВ: РЕЗУЛЬТАТЫ КИНЕМАТИЧЕСКОГО МОДЕЛИРОВАНИЯ
БРОНГУЛЕЕВ В.ВАД. — 2009 г.
Kinematic model of slope development includes terms concerning slope recession, slope flattening and tectonic movements. Different types of tectonic movements and base level reaction were used. The modelling shows that the preservation of characteristic features of slope profile ("memory of relief) depends on the ratio between the different slope processes intensity: the more the contribution of arid-type processes (sheet erosion, deflation) and the less the contribution of humid-type ones (ground's viscous flow) - the longer existence of characteristic details of the slope profile. Intermittent tectonic uprise leads to formation of the horizontal steps sequence (piedmont benchland) of different modes depending of base level conditions and tectonic movements character.
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НЕОТЕКТОНИКА И НЕФТЕНОСНОСТЬ ГЕОСТРУКТУР ТАТАРСТАНА
МИНГАЗОВ Б.М., МИНГАЗОВ М.Н. — 2009 г.
Spatial-varied neotectonic movements within the Tatarstan territory results in the rearrangement of the structural pattern of crystalline basement, sediment cover and day surface. The straight correlation is observed between oil reserves of geostructures and their neotectonic regime: the upward movements cause the inflow of oil-fluids from their generative origin to positive structures. The downcast movements lead to squeezing fluids from the structure.
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НОВЕЙШИЕ ДЕФОРМАЦИИ ГЕОЛОГИЧЕСКОЙ СТРУКТУРЫ АРХИПЕЛАГА ШПИЦБЕРГЕН (НОРВЕГИЯ)
ЗЫКОВ Д.С. — 2009 г.
By use of geomorphologic methods, the evidences of neotectonic activation of some local structures (thrusts, normal faults, and folds) on the archipelago Spitsbergen were found. The existing of morphostructures of compression is especially interesting, while in accordance with the prevalent view extension is the main characteristic of neotectonic regime of the area.
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О РАНГАХ ФОРМ РЕЛЬЕФА
НЕВСКИЙ В.Н. — 2009 г.
An attempt to analyse logically the taxonomic rank problem in geomorphology is undertaken. Since the rank criteria in the most of classifications are not determined the author suggests that the use of binary system of attributes -extensional and intensional ones (or extensive and intensive) would be efficient. For the process of inductive aggregation of the taxons of the second and higher ranks two rules are put forward, which distinctly raise objectivity of geomorphologic ranks definition.
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О СВОЙСТВАХ ГЕОМОРФОЛОГИЧЕСКИХ СИСТЕМ
МАККАВЕЕВ А.Н. — 2009 г.
Geomorphologic system (GMS) is the aggregate of topographic forms and elements interrelated by morphogenic processes, which possess emergent features and is characterized by inner activity. These are complex stochastic systems having the attributes of centrality of purpose and autoregulation. One of the research problems is to show that given complex of forms may be considered as a system and not as merely body or mix of elements, that this complex answers the main system principles among which integrity denominates self-sufficiency of this object, its distinctness. Geomorphic processes provide inner activity and self-sufficiency of GMS. The integrity means compactness of GMS, its space unity. GMSs may only be divided or united until they persist as integral geomorphologic units, until they posses such qualities as height (depth), length, slope, form of profile etc.
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ОБВАЛЫ И ОПОЛЗНИ ЮГА РОССИЙСКОГО ДАЛЬНЕГО ВОСТОКА
КОРОБОВ В.В., КОРОТКИЙ А.М., СКРЫЛЬНИК Г.П. — 2009 г.
The long-term study of landslides and landfalls was carried out in the different mountains of the southern Far East. The geographical, geological and geomorphologic methods were used, including geomorphologic mapping and drilling on some landslides complexes.
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ОБСУЖДЕНИЕ ОСНОВНЫХ ПОНЯТИЙ СИСТЕМНОГО ГЕОМОРФОЛОГИЧЕСКОГО АНАЛИЗА
2009
The paper represents the edited record of discussion of the main concepts of system geomorphologic analysis which took place in the laboratory of geomorphology IGRAS. Special attention was paid to the essence of the term geomorphologic system and its organization. Different opinions show the lack of consensus the necessity of which is obvious.
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ОПОЛЗНИ В ДОЛИНЕ НИЖНЕГО ТЕЧЕНИЯ Р. ЗЕИ: УСЛОВИЯ ФОРМИРОВАНИЯ, ОСОБЕННОСТИ РАЗВИТИЯ И МЕХАНИЗМ СМЕЩЕНИЯ
ГУСЕВ М.Н., ПОМИГУЕВ Ю.В. — 2009 г.
Slumping is one of the main geomorphic processes at the right side of Zeya River valley in its lower range. Investigation of volume and sliding mechanism of Malosazankovsky landslide occurred in November 1985 have shown that this landslide was composite one and may be considered as the largest one in the Russian Far East. A wide occurrence of landslides in the Zeya River valley determines in many respects the character of its channel formation.
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ОСОБЕННОСТИ МОРФОЛИТОГЕНЕЗА КАРСТОВЫХ БЕРЕГОВ КАМСКОГО ВОДОХРАНИЛИЩА
НАЗАРОВ Н.Н., ФРОЛОВА И.В. — 2009 г.
Leaching of underwater elements of gypsum banks causes the decreasing of the bench width. The activity of the leaching is comparable with the rate of cliffs abrasion. The volume of solid flow from the gypsum bank is tens and hundreds times less than that from the banks of the other rocks.