Ответственность: Мельников Павел Иванович (Редактор)
Издательство: Наука, Сибирское отделение
Год выпуска: 1986
Количество страниц: 180 с.
Шумилов, Юрий Васильевич.
Континентальный литогенез и россыпеобразование в криолитозоне / Ю. В. Шумилов ; ответственный редактор: П. И. Мельников ; Академия наук СССР, Сибирское отделение, Институт мерзлотоведения. - Новосибирск : Наука, Сибирское отделение, 1986. - 171, [2] с.
Издательство: Сахаполиграфиздат
Год выпуска: 2002
Количество страниц: 152 с.
Издательство: Наука, Сибирское предприятие РАН
Год выпуска: 1997
Количество страниц: 208 с.
Издательство: Якутский филиал, Сибирское отделение, Академия наук СССР
Год выпуска: 1981
Количество страниц: 148 с.
Магматизм, метасоматизм и литология рудных узлов Восточной и Южной Якутии : сборник научных трудов / Академия наук СССР, Якутский филиал, Институт геологии. - Якутск : Якутский филиал, Сибирское отделение, Академия наук СССР, 1981. - 140 с.
Количество страниц: 7 с.
The results of generalization and GIS integration of the results of the study of all known indigenous deposits and manifestations of diamonds located in the distributed and undistributed fund of the subsoil of the Russian Federation are presented. The work takes into account the results of prospecting, exploration and exploitation works, minutes of meetings of regional (TKZ) and federal (RKZ and GKZ) commissions on mineral reserves and published data. As a result, a GIS-integrated database was created containing 1,319 objects, for each of which key parameters were determined: coordinates, shape, size, age, average diamond content, forecast resources, and diamond reserves. It was established that the indigenous diamond deposits are concentrated in the Central Siberian subprovincia and account for 2.3 % of all known kimberlite bodies, diamond-bearing kimberlite bodies in the Yakut diamond-bearing province - 282, the predominant body shape is a pipe (59 %). There is no correlation between the size of kimberlite bodies and their diamond content, small pipes, as well as large diatremes, can be industrially diamondiferous, the prevailing absolute age of industrially diamondiferous kimberlites is 329-382 million years.
Шахурдина, Н. К. Геологическое картирование кимберлитового магматизма как фактурная оценка алмазоносных объектов Западной Якутии / Н.К. Шахурдина ; Акционерная компания "АЛРОСА" // Вестник Северо-Восточного федерального университета им. М. К. Аммосова. Серия "Науки о Земле". - 2024. - N 1 (33). - C. 68-74. - DOI: 10.25587/2587-8751-2024-1-68-74
DOI: 10.25587/2587-8751-2024-1-68-74
Количество страниц: 20 с.
A complex comparative study of diamonds from commercially productive diatremes of Daldyn- Alakitsky eld (Udachnaya, Zarnitsa) determined mineral typomorphic features, which allows diagnosing dispersion haloes of kimberlite material in sedimentary thick layers. By the set of typomorphic features, diamonds from Udachnaya pipe have many common features with crystals of other deposits of Daldyn-Alakitsky diamondiferous region. Increased content of variety II and III cubes, close by their features to diamonds from deep inclusions of eclogites, may be referred as inherent only to the Udachnaya pipe features. Zarnitsa pipe demonstarted pronounced prevalence of rhombic dodecahedral habit crystals of variety 1 with large concentration (> 30 %) of typically rounded diamonds. On the whole, diamonds of Daldyn eld are characterized by a complex of typomorphic features, which allow distinguishing them from diatremes of other diamondiferous regions of the Siberian platform with con dence.
Зинчук, Н. Н. Сравнительные особенности алмазов из кимберлитовых месторождений северной части Сибирской платформы / Н. Н.Зинчук, Л. Д. Бардухинов ; Академия наук Республики Саха (Якутия), Западно-Якутский научный центр // Вестник Северо-Восточного федерального университета им. М. К. Аммосова. Серия: "Наука о земле". - 2024. - N 1 (33). - C. 11-30. - DOI: 10.25587/2587-8751-2024-1-11-30
DOI: 10.25587/2587-8751-2024-1-11-30
Издательство: Книжное издательство
Год выпуска: 1974
Количество страниц: 190 с.
Количество страниц: 8 с.
The northern slope of the Yakut uplift covers the North Aldan oil and gas bearing region and partially the Pre-Verkhoyansk and Vilyui oil and gas bearing regions. The potential oil and gas content of the Northern slope of the Yakut uplift is associated with a wide stratigraphic range of promising sediment complexes (Vendian-Cambrian, Permian-Triassic and Jurassic-Cretaceous). All these complexes have confirmed oil or gas occurrences of varying intensity. Terrigenous-carbonate formations of the Vendian-Cambrian complex are the most promising deposits in terms of oil and gas potential, confined to the lower part of the upper sub-suite of the Yudom formation of the Vendian. A relatively effective fluid seals for the Vendian hydrocarbons can be the variegated formation of the Lower Cambrian, composed of dense mudded-off carbonate rocks. The prospects of Permian-Triassic and Jurassic-Cretaceous sediment complexes will be determined by the absence or presence of zonal and local fluid seals, including non-traditional permafrost hydrate. Thus, several oil and gas complexes of different origin and with different types of fluid seals are identified in the section. A brief overview of the promising oil and gas complexes of the Northern slope of the Yakut uplift emphasizes the need for priority geological exploration for oil and gas. Clarification of geological structure of the studied area will make it possible to identify the most promising zones and sites for planning and organzing exploration work. The work was carried out with financial support within the framework of the State Assignment of the Ministry of Science and Higher Education of the Russian Federation No. 122011100158-1 using scientific equipment of the Center for Collective Use of the Federal research center "Yakut Scientific Center of the Siberian Branch of the Russian Academy of Sciences" within the framework of grant No. 13.TsKP.21.0016.
Калинин, А. И. Перспективные нефтегазоносные комплексы на северном склоне Якутского поднятия / Калинин А. И. ; Институт проблем нефти и газа // Успехи современного естествознания. - 2023. - N 12. - С. 185-192. - DOI: 10.17513/use.38190
DOI: 10.17513/use.38190
Количество страниц: 6 с.
The article examines the influence of the Elga Coal Complex (ECC) on the hydrochemical state of surface waters. Open-pit mining of the Elga coal deposit takes place on the watershed of the Mulam and Algoma rivers, which are part of the hydrographic network of the Uchur river. During field work in 2012-2019, water samples for analysis were taken in two areas: on the right tributaries of the Algoma river and Bolshoye Toko Lake. Based on the analysis of selected samples, a new hydrochemical composition of water bodies was identified based on generally accepted methods in the Russian Federation. All samples had exceeded the maximum permissible concentrations for water bodies of fishery importance (MPCf), except for Lake Bolshoye Toko. The identified changes are presumably seasonal. In winter the flow on the tributaries of the Algoma and Mulam completely stops or decreases to vanishingly small values. To identify patterns in the formation of the qualitative state of water bodies in the zone affected by open-pit coal mining in permafrost conditions, further systematic observations are required until the planned production of high-quality coal oriented for export is achieved. The work was carried out within the framework of the state assignment of the Ministry of Science and Higher Education of the Russian Federation No. FWRS-2021-0014.
Изменение гидрохимического состояния поверхностных вод в зоне воздействия Эльгинского угольного комплекса (2012-2019 гг.) / Ноговицын Д. Д., Никулин К. В., Сергеева Л. П. [и др.] ; Институт физико-технических проблем Севера им. В. П. Ларионова // Успехи современного естествознания. - 2023. - N 11. - С. 168-173. - DOI: 10.17513/use.38159
DOI: 10.17513/use.38159